مجله زمین شناسی نفت ایران، سال پنجم، شماره 9

1. ‫رﯾﺰ‬‫رﺧﺴﺎره‬‫ﻫﺎ‬‫و‬‫ﻣﺪل‬‫رﺳﻮﺑﯽ‬‫ﺳﺎزﻧﺪ‬‫آﺳﻤﺎري‬)‫اﻟﯿﮕﻮﺳﻦ‬(‫در‬‫ﺷﻤﺎل‬‫ﻏﺮب‬‫روﺳﺘﺎي‬‫درﯾﺲ‬...
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‫ر‬‫ﯾ‬‫ﺰ‬‫رﺧﺴﺎره‬‫ﻫﺎ‬‫و‬‫ﻣﺪل‬‫رﺳﻮﺑﯽ‬‫ﺳﺎزﻧﺪ‬‫آﺳﻤﺎري‬)‫اﻟ‬‫ﯿ‬‫ﮕﻮﺳﻦ‬(‫در‬‫ﺷﻤﺎل‬‫ﻏﺮب‬
‫روﺳﺘﺎي‬‫در‬‫ﯾ‬‫ﺲ‬)‫ﻏﺮب‬‫اﺳﺘﺎن‬‫ﻓﺎرس‬(‫و‬‫ﻣﻘﺎ‬‫ﯾ‬‫ﺴﻪ‬،‫ﺿﺨﺎﻣﺖ‬‫ﺳﻦ‬‫و‬‫ﻣﺤ‬‫ﯿ‬‫ﻂ‬‫رﺳﻮﺑﯽ‬
‫ﺑﺎ‬‫ﺳﻪ‬‫ﺑﺮش‬‫د‬‫ﯾ‬‫ﮕﺮ‬‫در‬‫ﺣﻮﺿﻪ‬‫زاﮔﺮس‬
‫در‬‫ﯾ‬‫ﺎﻓﺖ‬‫آذر‬1394‫ﭘﺬ‬ ،‫ﯾ‬‫ﺮش‬‫ﺑﻬﻤﻦ‬4139
‫ﭼﮑ‬‫ﯿ‬‫ﺪه‬
‫در‬‫اﯾﻦ‬‫ﺗﺤﻘﯿﻖ‬‫رﯾﺰ‬‫رﺧﺴﺎره‬‫ﻫﺎ‬‫و‬‫ﻣﺪل‬‫رﺳﻮﺑﯽ‬‫ﺳﺎزﻧﺪ‬‫آﺳﻤﺎري‬‫ﺑﻪ‬‫ﺳﻦ‬‫اﻟﯿﮕﻮﺳﻦ‬)‫روﭘﻠﯿﻦ‬-‫ﺷﺎﺗﯿﻦ‬(‫در‬‫ﺷﻤﺎل‬‫ﻏﺮب‬‫روﺳﺘﺎي‬
،‫درﯾﺲ‬‫واﻗﻊ‬‫در‬‫زون‬‫ﻓﺎرس‬‫داﺧﻠﯽ‬‫ﺣﻮﺿﻪ‬،‫زاﮔﺮس‬‫ﺑﺮرﺳﯽ‬‫و‬‫ﺗﻔﺴﯿﺮ‬‫ﮔﺮدﯾﺪه‬‫اﺳﺖ‬.‫ﻣﺨﺘﺼﺎت‬‫ﺟﻐﺮاﻓﯿﺎﯾﯽ‬‫اﯾﻦ‬‫ﺑﺮش‬"26'32
°51‫ﺷﺮﻗﯽ‬‫و‬"59'41°29‫ﺷﻤﺎﻟﯽ‬‫ﻣﯽ‬‫ﺑﺎﺷﺪ‬.‫ﻧﻬﺸﺘﻪ‬‫ﻫﺎي‬‫ﺳﺎزﻧﺪ‬‫آﺳﻤﺎري‬‫در‬‫ﺑﺮش‬‫درﯾﺲ‬‫ﺑﻪ‬5‫واﺣﺪ‬‫ﺳﻨﮓ‬‫ﭼﯿﻨﻪ‬‫ﻧﮕﺎري‬‫ﺗﻘﺴﯿﻢ‬
‫ﻣﯽ‬‫ﺷﻮﻧﺪ‬‫ﮐﻪ‬‫ﺷﺎﻣﻞ‬460‫ﻣﺘﺮ‬‫آﻫﮏ‬‫ﺧﺎﮐﺴﺘﺮي‬‫و‬‫ﮐﺮم‬‫ﻣﺘﻤﺎﯾﻞ‬‫ﺑﻪ‬‫ﺧﺎﮐﺴﺘﺮي‬،‫ﻧﺎزك‬،‫ﻣﺘﻮﺳﻂ‬‫ﺿﺨﯿﻢ‬‫و‬‫ﺗﻮده‬‫اي‬‫و‬ً‫ﺎ‬‫ﺑﻌﻀ‬‫دوﻟﻮ‬‫ﻣﯿﺘﯽ‬
‫ﺑﺎ‬‫ﻣﯿﺎن‬‫ﻻﯾﻪ‬‫ﻫﺎي‬‫ﻣﺎرﻧﯽ‬‫ﻣﯽ‬‫ﺑﺎﺷﺪ‬.‫ﺑﺎ‬‫ﻣﻄﺎﻟﻌﻪ‬‫ﮔﻮﻧﻪ‬-‫ﻫﺎي‬‫ﻓﺮاﻣﯿﻨﯿﻔﺮﻫﺎي‬‫ﮐﻒ‬‫زي‬‫و‬‫ﻏﯿﺮ‬،‫ﻓﺮاﻣﯿﻨﯿﻔﺮﻫﺎ‬‫و‬‫ﺑﺮرﺳﯽ‬‫وﯾﮋﮔﯽ‬‫ﻫ‬‫ﺎﯾﯽ‬‫از‬‫ﻗﺒﯿﻞ‬
‫اﺟﺘﻤﺎع‬‫ﻋﻨﺎﺻﺮ‬‫اﺳﮑﻠﺘﯽ‬‫و‬‫ﺑﺎﻓﺖ‬‫رﺳﻮﺑﯽ‬‫ﻣﻘﺎﻃﻊ‬،‫ﻣﯿﮑﺮوﺳﮑﻮﭘﯽ‬14‫رﯾﺰ‬‫رﺧﺴﺎره‬‫ﺑﺮاي‬‫ﺳﺎزﻧﺪ‬‫آﺳﻤﺎري‬‫ﻣﻌﺮﻓﯽ‬‫ﺷﺪه‬‫اﺳﺖ‬.‫ﺗﻐﯿﯿﺮات‬
‫ﺗﺪرﯾﺠﯽ‬‫ﻋﻤﻮدي‬‫اﯾﻦ‬‫رﯾﺰ‬‫رﺧﺴﺎره‬‫ﻫﺎ‬‫ﺣﺎﮐﯽ‬‫از‬‫ﺗﻪ‬‫ﻧﺸﺴﺖ‬‫رﺳﻮﺑﺎت‬‫ﺳﺎزﻧﺪ‬‫آﺳﻤﺎري‬‫در‬‫ﯾﮏ‬‫رﻣﭗ‬‫ﻫﻤﻮﮐﻠﯿﻨﺎل‬‫ﻣﯽ‬‫ﺑﺎﺷﺪ‬.‫اﯾﻦ‬
‫رﻣﭗ‬‫ﻫﻤﻮﮐﻠﯿﻨﺎل‬‫ﺷﺎﻣﻞ‬‫رﻣﭗ‬‫ﻣﯿﺎﻧﯽ‬‫و‬‫رﻣﭗ‬‫دروﻧﯽ‬‫ﺑﻮده‬‫ﮐﻪ‬‫اﯾﻦ‬‫دو‬‫ﺑﺨﺶ‬‫ﺗﻮﺳﻂ‬‫ﻣﺤﯿﻂ‬‫ﺳﺪ‬‫از‬‫ﻫﻢ‬‫ﺟﺪا‬‫ﻣﯽ‬‫ﺷﻮﻧﺪ‬.‫رﻣﭗ‬‫ﻣﯿﺎﻧﯽ‬
‫ﺑﺎ‬‫ﺣﻀﻮر‬‫و‬‫ﻓﺮاواﻧﯽ‬‫ﻓﺮاﻣﯿﻨﯿﻔﺮﻫﺎي‬‫ﻫﯿﺎﻟﯿﻦ‬‫ﮐﻒ‬،‫زي‬‫ﺟﻠﺒﮏ‬‫ﻗﺮﻣﺰ‬‫ﮐﻮراﻟﯿﻨﺎﺳﻪ‬‫آ‬‫و‬‫اﮐﯿﻨﻮﺋﯿﺪ‬‫ﻣﻌﺮﻓﯽ‬‫ﻣﯽ‬‫ﮔﺮدد‬.‫ﻫﻤﭽﻨﯿﻦ‬‫ﻣﻬﻢ‬‫ﺗﺮﯾﻦ‬
‫ﺧﺮده‬‫ﻫﺎي‬‫اﺳﮑﻠﺘﯽ‬‫رﻣﭗ‬‫دروﻧﯽ‬‫ﻓﺮاﻣﯿﻨﯿﻔﺮﻫﺎي‬‫ﭘﺮﺳﻼﻧﻮز‬‫ﻣﯽ‬‫ﺑﺎﺷﻨﺪ‬.‫ﺑﻪ‬‫ﻣﻨﻈﻮر‬‫ﻣﻘﺎﯾﺴﻪ‬،‫ﺿﺨﺎﻣﺖ‬‫ﺳﻦ‬‫و‬‫ﻣﺤﯿﻂ‬‫ﻫﺎي‬‫رﺳﻮ‬،‫ﺑﯽ‬
‫ﺗﻄﺎﺑﻖ‬‫ﻧﺎﺣﯿﻪ‬‫اي‬‫ﺳﺎزﻧﺪ‬‫آﺳﻤﺎري‬‫در‬‫ﺑﺮش‬‫درﯾﺲ‬‫ﺑﺎ‬‫ﺳﻪ‬‫ﺑﺮش‬‫دﯾﮕﺮ‬)‫ﺑﺮش‬‫ﺗﺎﻗﺪﯾﺲ‬،‫ﻧﺎاورا‬‫ﺑﺮش‬‫ﺗﺎﻗﺪﯾﺲ‬‫دﯾﻞ‬‫و‬‫ﺑﺮش‬‫د‬‫ﻫﻠﺮان‬(،
‫در‬‫ﺣﻮﺿﻪ‬‫زاﮔﺮس‬‫اﻧﺠﺎم‬‫ﺷﺪه‬‫اﺳﺖ‬.‫اﯾﻦ‬‫ﺗﻄﺎﺑﻖ‬‫ﺑﯿﺎن‬‫ﮐﻨﻨﺪه‬‫ﺟﻮان‬‫ﺗﺮ‬‫ﺷﺪن‬‫ﺳﻦ‬‫ﺳﺎزﻧﺪ‬‫آﺳﻤﺎري‬‫ﺑﻪ‬‫ﺳﻤﺖ‬‫ﺑﺨﺶ‬‫ﻫﺎي‬‫ﻋﻤﯿﻖ‬‫ﺗ‬‫ﺮ‬
‫ﺣﻮﺿﻪ‬‫ﻓﻮرﻟﻨﺪ‬‫زاﮔﺮس‬‫ﻣﯽ‬‫ﺑﺎﺷﺪ‬.
‫ﮐﻠ‬ ‫ﮐﻠﻤﺎت‬‫ﯿ‬‫ﺪ‬‫ي‬:‫ﺣﻮﺿﻪ‬،‫زاﮔﺮس‬‫ﻓﺎرس‬،‫داﺧﻠﯽ‬‫ﺳﺎزﻧﺪ‬،‫آﺳﻤﺎري‬،‫اﻟﯿﮕﻮﺳﻦ‬‫رﯾﺰ‬،‫رﺧﺴﺎره‬‫رﻣﭗ‬‫ﻫﻤﻮﮐﻠﯿﻨﺎل‬.

2. ‫رﯾﺰ‬‫رﺧﺴﺎره‬‫ﻫﺎ‬‫و‬‫ﻣﺪل‬‫رﺳﻮﺑﯽ‬‫ﺳﺎزﻧﺪ‬‫آﺳﻤﺎري‬)‫اﻟﯿﮕﻮﺳﻦ‬(‫در‬‫ﺷﻤﺎل‬‫ﻏﺮب‬‫روﺳﺘﺎي‬‫درﯾﺲ‬...
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1.‫ﻣﻘﺪﻣﻪ‬
‫ﺳﺎزﻧﺪ‬‫آﺳﻤﺎري‬‫ﺗﻮاﻟﯽ‬‫ﺿﺨﯿﻤﯽ‬‫از‬‫ﺳﻨﮓ‬‫ﻫﺎي‬‫ﮐﺮﺑﻨﺎﺗﻪ‬‫اﻟﯿﮕﻮ‬-‫ﻣﯿﻮﺳﻦ‬‫اﺳﺖ‬.‫ﮐﺮﺑﻨﺎت‬¬‫ﻫﺎي‬‫اﯾﻦ‬‫ﺳﺎزﻧﺪ‬‫و‬‫ﺑﺨﺶ‬‫ﻣﺎﺳﻪ‬‫ﺳ‬‫ﻨﮕﯽ‬‫آن‬
‫ﺣﺎوي‬‫ﻧﻔﺖ‬‫و‬‫ﮔﺎز‬‫ﺑﻮده‬‫ﺑﻪ‬‫ﻃﻮري‬‫ﮐﻪ‬‫اﯾﻦ‬‫ﺳﺎزﻧﺪ‬‫ﻣﻬﻢ‬‫ﺗﺮﯾﻦ‬‫ﺳﻨﮓ‬‫ﻣﺨﺰن‬‫در‬‫ﺣﻮﺿﻪ‬‫زاﮔﺮس‬‫ﻣﺤﺴﻮب‬‫ﻣﯽ‬‫ﺷﻮد‬)،‫ﺻﯿﺮﻓﯿﺎن‬
1386.(‫ﻧﺎم‬‫اﯾﻦ‬‫ﺳﺎزﻧﺪ‬‫از‬‫ﮐﻮه‬،‫آﺳﻤﺎري‬‫واﻗﻊ‬‫در‬‫ﺷﻤﺎل‬‫ﺷﺮق‬‫ﺷﻬﺮﺳﺘﺎن‬‫ﻣﺴﺠﺪ‬‫ﺳﻠﯿﻤﺎن‬‫اﻗﺘﺒﺎس‬‫ﺷﺪه‬‫اﺳﺖ‬)،‫آﻗﺎﻧﺒﺎﺗﯽ‬1383.(‫ﺑﻪ‬
‫ﻋﻠﺖ‬‫ﻣﻘﺎوﻣﺖ‬‫و‬‫ﺳﺨﺘﯽ‬‫ﺧﺎص‬‫آﻫﮏ‬‫ﻫﺎي‬‫ﺳﺎزﻧﺪ‬،‫آﺳﻤﺎري‬‫اﯾﻦ‬‫ﺳﺎزﻧﺪ‬‫ارﺗﻔﺎﻋﺎت‬‫و‬‫ﺑﺨﺶ‬‫ﻫﺎي‬‫ﻣﻘﺎوم‬‫ﻣﻨﻄﻘﻪ‬‫زاﮔﺮس‬‫ﭼﯿﻦ‬‫ﺧﻮرده‬
‫را‬‫ﺗﺸﮑﯿﻞ‬‫ﻣﯽ‬‫دﻫﺪ‬)‫دروﯾﺶ‬،‫زاده‬1388.(‫اﯾﻦ‬‫ﺳﺎزﻧﺪ‬‫در‬‫ﺑﺮش‬‫ﻫﺎي‬‫ﮐﺎﻣﻞ‬‫ﺑﻪ‬‫دو‬‫ﺑﺨﺶ‬‫ﻋﻀﻮ‬‫ﻣﺎﺳﻪ‬‫ﺳﻨﮓ‬‫اﻫﻮاز‬‫در‬‫ﻧﻮاﺣﯽ‬
‫ﺟﻨﻮﺑﯽ‬‫ﻓﺮواﻓﺘﺎدﮔﯽ‬‫دزﻓﻮل‬‫و‬‫ﻋﻀﻮ‬‫ﺗﺒﺨﯿﺮي‬‫ﮐﻠﻬﺮ‬‫در‬‫ﺟﻨﻮب‬‫ﻏﺮب‬‫ﻟﺮﺳﺘﺎن‬‫ﺗﻘﺴﯿﻢ‬‫ﻣﯽ‬‫ﺷﻮد‬)،‫ﻣﻄﯿﻌﯽ‬1372(‫و‬‫در‬‫زﻣﺎن‬‫اﻟﯿﮕﻮﺳﻦ‬
‫ﺗﺎ‬،‫ﻣﯿﻮﺳﻦ‬‫در‬‫ﺣﻮﺿﻪ‬‫ﻓﻮرﻟﻨﺪ‬‫زاﮔﺮس‬‫ﺗﺸﮑﯿﻞ‬‫ﺷﺪه‬‫اﺳﺖ‬)،‫ﻋﻠﻮي‬2004(.‫روزن‬‫داران‬‫ﻧﺸﺎﻧﮕﺮﻫﺎي‬‫ﻣﺤﯿﻄﯽ‬‫ﺧﻮﺑﯽ‬‫ﻣﺤﺴﻮب‬‫ﻣﯽ‬
‫ﺷﻮﻧﺪ‬‫و‬‫اﻏﻠﺐ‬‫ﻣﯽ‬‫ﺗﻮان‬‫از‬‫آن‬‫ﻫﺎ‬‫در‬‫ﺑﺎزﺳﺎزي‬‫ﻣﺤﯿﻂ‬‫و‬‫ﺗﻐﯿﯿﺮات‬‫ﺳﻄﺢ‬‫آب‬‫درﯾﺎ‬‫اﺳﺘﻔﺎده‬‫ﮐﺮد‬)،‫ﮔﯿﻞ‬2000.(‫ﺣﺴﺎس‬‫ﺑﻮدن‬‫ﺑﻪ‬
‫ﮐﻨﺘﺮل‬‫ﮐﻨﻨﺪه‬‫ﻫﺎي‬‫اﮐﻮﻟﻮژﯾﮑﯽ‬‫از‬‫ﻗﺒﯿﻞ‬:‫ﻋﻤﻖ‬‫ﻣﺤﯿﻂ‬‫و‬‫ﻓﺸﺎر‬،‫ﻫﯿﺪروﺳﺘﺎﺗﯿﮏ‬‫اﻧﺮژي‬،‫ﻫﯿﺪروﻟﯿﮑﯽ‬،‫دﻣﺎ‬‫ﻧﻮر‬‫و‬‫ﺗﻮرﺑﯿﺪﯾﺘ‬،‫ﻪ‬‫ﻣﻮاد‬،‫ﻏﺬاﯾﯽ‬
،‫ﺷﻮري‬‫ﻣﺎﻫﯿﺖ‬‫ﮐﻒ‬‫ﺣﻮﺿﻪ‬،‫رﺳﻮﺑﯽ‬‫ﻣﯿﺰان‬‫ﮔﺎز‬O2‫و‬PH،‫ﻣﺤﯿﻂ‬‫و‬‫ﻫﻤﭽﻨﯿﻦ‬‫داﺷﺘﻦ‬‫وﯾﮋﮔﯽ‬‫ﻫﺎﯾﯽ‬‫ﻧﻈﯿﺮ‬:‫ﭼﺮﺧﻪ‬‫زﻧﺪﮔﯽ‬،‫ﮐﻮﺗﺎه‬
‫ﺗﻨﻮع‬،‫زﯾﺎد‬‫ﻓﺮاواﻧﯽ‬‫ﺑﺎﻻ‬‫و‬‫ﺣﻔﻆ‬‫ﺷﺪﮔﯽ‬‫در‬‫رﺳﻮﺑﺎت‬‫ﻣﻮﺟﺐ‬‫ﺷﺪه‬‫اﺳﺖ‬‫ﮐﻪ‬‫ﻓﺮاﻣﯿﻨﯿﻔﺮﻫﺎي‬‫ﺳﻨﮕﻮاره‬‫ﺷﺎﺧﺺ‬‫ﺗﺮﯾﻦ‬‫ﻧﺸﺎﻧ‬‫ﻪ‬‫ﻫﺎي‬
‫دﯾﺮﯾﻨﻪ‬-‫ﻣﺤﯿﻄﯽ‬‫در‬‫ﭘﻼﺗﻔﺮم‬‫ﻫﺎي‬‫ﮐﺮﺑﻨﺎﺗﻪ‬‫ﺳﻨﻮزوﺋﯿﮏ‬‫ﻣﺤﺴﻮب‬‫ﺷﻮﻧﺪ‬.‫ﺑﺎ‬‫ﻣﻄﺎﻟﻌﻪ‬‫ﻓﺮاﻣﯿﻨﯿﻔﺮﻫﺎ‬‫در‬‫ﻣﻘﺎﻃﻊ‬‫ﻧﺎزك‬‫ﻣﯿﮑﺮ‬‫وﺳﮑﻮﭘﯽ‬‫و‬
‫ﺷﻨﺎﺳﺎﯾﯽ‬‫رﯾﺰ‬‫رﺧﺴﺎره‬،‫ﻫﺎ‬‫ﺷﺮاﯾﻂ‬‫ﻣﺤﯿﻄﯽ‬‫زﻣﺎن‬‫ﺗﻪ‬‫ﻧﺸﺴﺖ‬‫رﺳﻮﺑﺎت‬‫ﮐﺮﺑﻨﺎﺗﻪ‬‫را‬‫ﻣﯿﺘﻮان‬‫ﺗﻔﺴﯿﺮ‬‫ﮐﺮد‬.
2.‫ﻣﻄﺎﻟﻌﻪ‬ ‫روش‬
‫در‬ ‫درﯾﺲ‬ ‫روﺳﺘﺎي‬ ‫ﺣﻮاﻟﯽ‬ ‫در‬ ‫ﻣﻄﺎﻟﻌﻪ‬ ‫ﺑﺮش‬7‫ـ‬ ‫ﮐﺎزرون‬ ‫ﺟﺎده‬ ‫ﻣﺴﯿﺮ‬ ‫از‬ ‫و‬ ‫ﺷﺪه‬ ‫واﻗﻊ‬ ‫ﮐﺎزرون‬ ‫ﺷﻬﺮﺳﺘﺎن‬ ‫ﻏﺮب‬ ‫ﺷﻤﺎل‬ ‫ﮐﯿﻠﻮﻣﺘﺮي‬
‫)ﺷﮑﻞ‬ ‫اﺳﺖ‬ ‫دﺳﺘﺮﺳﯽ‬ ‫ﻗﺎﺑﻞ‬ ‫ﻓﺎرس‬ ‫اﺳﺘﺎن‬ ‫ﻏﺮب‬ ‫در‬ ‫ﻗﺎﺋﻤﯿﻪ‬ ‫ـ‬ ‫درﯾﺲ‬1‫ﺷﻤﺎل‬ ‫دﻣﺎﻏﻪ‬ ‫در‬ ‫درﯾﺲ‬ ‫ﺑﺮش‬ .(‫و‬ ‫ﺳﺮﺑﺎﻟﺶ‬ ‫ﺗﺎﻗﺪﯾﺲ‬ ‫ﻏﺮﺑﯽ‬
.‫اﺳﺖ‬ ‫ﺷﺪه‬ ‫واﻗﻊ‬ ‫آن‬ ‫ﺷﻤﺎﻟﯽ‬ ‫ﯾﺎل‬ ‫در‬"26'32o
51‫و‬ ‫ﺷﺮﻗﯽ‬"59'41o
29‫ﻣﯽ‬ ‫ﺑﺮش‬ ‫اﯾﻦ‬ ‫ﺟﻐﺮاﻓﯿﺎﯾﯽ‬ ‫ﻣﺨﺘﺼﺎت‬ ،‫ﺷﻤﺎﻟﯽ‬‫از‬ .‫ﺑﺎﺷﺪ‬
‫ﺗﻮاﻟﯽ‬ ،‫ﺟﻐﺮاﻓﯿﺎﯾﯽ‬ ‫ﻣﻮﻗﻌﯿﺖ‬ ‫ﻧﻈﺮ‬.‫دارد‬ ‫ﻗﺮار‬ ‫زاﮔﺮس‬ ‫داﺧﻠﯽ‬ ‫ﻓﺎرس‬ ‫زون‬ ‫در‬ ‫ﻣﺮﺑﻮﻃﻪ‬ ‫ﺑﺮش‬ ‫ﺳﺎﺧﺘﻤﺎﻧﯽ‬ ‫وﺿﻌﯿﺖ‬ ‫و‬ ‫رﺳﻮﺑﯽ‬ ‫ﻫﺎي‬‫ﺑ‬‫ﺮ‬
‫ﺑﺎ‬ ‫و‬ ‫ﺻﺤﺮاﯾﯽ‬ ‫ﻣﻄﺎﻟﻌﺎت‬ ‫اﺳﺎس‬‫ﻻﯾﻪ‬ ‫ﺿﺨﺎﻣﺖ‬ ‫ﺑﻪ‬ ‫ﺗﻮﺟﻪ‬‫ﻓﻮاﺻﻞ‬ ‫ﺑﺎ‬ ‫ﺑﺮداري‬ ‫ﻧﻤﻮﻧﻪ‬ ،‫ﻓﺴﯿﻠﯽ‬ ‫آﺛﺎر‬ ‫و‬ ‫رﻧﮓ‬ ،‫ﻟﯿﺘﻮﻟﻮژي‬ ،‫ﻫﺎ‬1‫ﺗﺎ‬2‫ﻣﺘﺮي‬
‫از‬ ‫و‬ ‫ﺷﺪ‬ ‫اﻧﺠﺎم‬ ‫ﺳﯿﺴﺘﻤﺎﺗﯿﮏ‬ ‫ﺻﻮرت‬ ‫ﺑﻪ‬460،‫آﺳﻤﺎري‬ ‫ﺳﺎزﻧﺪ‬ ‫ﺿﺨﺎﻣﺖ‬ ‫ﻣﺘﺮ‬450‫ﺷﻤﺎره‬ ‫و‬ ‫ﺑﺮداﺷﺖ‬ ‫ﻧﻤﻮﻧﻪ‬‫از‬ ‫ﮐﻪ‬ ‫ﮔﺮدﯾﺪ‬ ‫ﮔﺬاري‬
‫ﺗﻌﺪاد‬ ‫ﻣﻘﺪار‬ ‫اﯾﻦ‬272‫ﻣ‬ .‫ﺷﺪ‬ ‫ﺗﻬﯿﻪ‬ ‫ﻣﯿﮑﺮوﺳﮑﻮﭘﯽ‬ ‫ﻣﻄﺎﻟﻌﺎت‬ ‫ﻣﻨﻈﻮر‬ ‫ﺑﻪ‬ ‫ﻧﺎزك‬ ‫ﻣﻘﻄﻊ‬‫ﺑﻪ‬ ‫آﺳﻤﺎري‬ ‫ﺳﺎزﻧﺪ‬ ‫ﻓﻮﻗﺎﻧﯽ‬ ‫و‬ ‫ﺗﺤﺘﺎﻧﯽ‬ ‫ﺮزﻫﺎي‬
‫ﻣﯽ‬ ‫ﭘﻮﺷﯿﺪه‬ ‫ﺻﻮرت‬‫ﺑﻪ‬ ‫درﯾﺲ‬ ‫ﺑﺮش‬ ‫در‬ ‫آﺳﻤﺎري‬ ‫ﺳﺎزﻧﺪ‬ .‫ﺑﺎﺷﺪ‬5‫ﺳﻨﮓ‬ ‫واﺣﺪ‬‫ﭼﯿﻨﻪ‬‫ﻣﯽ‬ ‫ﺗﻘﺴﯿﻢ‬ ‫ﻧﮕﺎري‬‫ﺣﺎﺻﻞ‬ ‫ﻧﺘﺎﯾﺞ‬ ‫ﻫﻤﭽﻨﯿﻦ‬ .‫ﺷﻮد‬
‫زﯾﺴﺖ‬ ‫ﻣﻄﺎﻟﻌﻪ‬ ‫از‬‫ﭼﯿﻨﻪ‬‫ﺑﯿﻮزون‬ ‫ﺷﻨﺎﺳﺎﯾﯽ‬ ‫ﺑﻪ‬ ‫ﻣﻨﺠﺮ‬ ‫ﻗﺒﻠﯽ‬ ‫ﻣﻄﺎﻟﻌﺎت‬ ‫در‬ ‫ﺑﺮش‬ ‫اﯾﻦ‬ ‫ﻧﮕﺎري‬‫ﻫﺎي‬Nummulites vascus-Nummulites
fichteli assemblage zone (Rupelian)‫و‬Archaias asmaricus-Archaias hensoni-Miogypsinoides
complanatus assemblage zone (Chattian)،‫ﻫﻤﮑﺎران‬ ‫و‬ ‫)اﺧﺰري‬ ‫اﺳﺖ‬ ‫ﮔﺮدﯾﺪه‬1394‫ﺳﺎزﻧﺪ‬ ‫ﺗﺸﮑﯿﻞ‬ ‫ﺑﯿﺎﻧﮕﺮ‬ ‫ﮐﻪ‬ ‫(؛‬
‫ﻣﯽ‬ (‫ﺷﺎﺗﯿﻦ‬ ‫ـ‬ ‫)روﭘﻠﯿﻦ‬ ‫اﻟﯿﮕﻮﺳﻦ‬ ‫زﻣﺎن‬ ‫در‬ ‫آﺳﻤﺎري‬،‫ﻫﻤﮑﺎران‬ ‫و‬ ‫)ﻻرﺳﻦ‬ ‫ﺑﺎﺷﺪ‬2009‫ون‬ ‫؛‬‫ﺑﻮﺧﻢ‬،‫ﻫﻤﮑﺎران‬ ‫و‬2010‫ﺣﺎﺿﺮ‬ ‫ﻣﻄﺎﻟﻌﻪ‬ .(
‫رﺧﺴﺎره‬ ‫رﯾﺰ‬ ‫ﺑﻪ‬‫ﻣﯽ‬ ‫ﻣﻄﺎﻟﻌﻪ‬ ‫ﻣﻮرد‬ ‫ﺑﺮش‬ ‫در‬ ‫ﮐﺮﺑﻨﺎﺗﻪ‬ ‫ﭘﻼﺗﻔﺮم‬ ‫در‬ ‫آﺳﻤﺎري‬ ‫ﺳﺎزﻧﺪ‬ ‫ﺗﺸﮑﯿﻞ‬ ‫ﭼﮕﻮﻧﮕﯽ‬ ‫و‬ ‫ﻫﺎ‬.‫ﭘﺮدازد‬

3. ‫رﯾﺰ‬‫رﺧﺴﺎره‬‫ﻫﺎ‬‫و‬‫ﻣﺪل‬‫رﺳﻮﺑﯽ‬‫ﺳﺎزﻧﺪ‬‫آﺳﻤﺎري‬)‫اﻟﯿﮕﻮﺳﻦ‬(‫در‬‫ﺷﻤﺎل‬‫ﻏﺮب‬‫روﺳﺘﺎي‬‫درﯾﺲ‬...
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‫ﺷﮑﻞ‬1‫راه‬ ‫ﻧﻘﺸﻪ‬ :،‫ﻣﺴﻠﺢ‬ ‫ﻧﯿﺮوﻫﺎي‬ ‫ﺟﻔﺮاﻓﯿﺎﯾﯽ‬ ‫)ﺳﺎزﻣﺎن‬ ‫ﻓﺎرس‬ ‫اﺳﺘﺎن‬ ‫ﻏﺮب‬ ‫در‬ ‫درﯾﺲ‬ ‫ﺑﺮش‬ ‫ﺷﻨﺎﺳﯽ‬ ‫زﻣﯿﻦ‬ ‫و‬ ‫دﺳﺘﺮﺳﯽ‬ ‫ﻫﺎي‬1384‫و‬ ‫ﻣﮑﻠﺌﻮد‬ ‫؛‬
،‫ﻣﺎﺟﺪي‬1972.(
3.‫ﺑﺤﺚ‬
4-1-‫رﺧﺴﺎره‬ ‫رﯾﺰ‬‫ﻫﺎ‬
) ‫داﻧﻬﺎم‬ ‫ﺑﻨﺪي‬ ‫ﻃﺒﻘﻪ‬ ‫اﺳﺎس‬ ‫ﺑﺮ‬ ‫ﻣﯿﮑﺮوﺳﮑﻮﭘﯽ‬ ‫ﻣﻘﺎﻃﻊ‬ ‫رﺳﻮﺑﯽ‬ ‫ﺑﺎﻓﺖ‬ ‫ﻣﻄﺎﻟﻌﻪ‬ ‫ﺗﺤﻘﯿﻖ‬ ‫اﯾﻦ‬ ‫در‬1962) ‫ﮐﻠﻮان‬ ‫و‬ ‫اﻣﺒﺮي‬ ،(1971‫راﯾﺖ‬ ‫و‬ (
)1992‫رﺧﺴﺎره‬ ‫رﯾﺰ‬ ‫ﺗﻔﺴﯿﺮ‬ ‫ﻫﻤﭽﻨﯿﻦ‬ ‫و‬ () ‫ﮔﯿﻞ‬ ‫ﻣﻄﺎﻟﻌﺎت‬ ‫اﺳﺎس‬ ‫ﺑﺮ‬ ‫ﻫﺎ‬2000) ‫ﻓﻠﻮﮔﻞ‬ ‫و‬ (2010.‫اﺳﺖ‬ ‫ﮔﺮدﯾﺪه‬ ‫اﻧﺠﺎم‬ (‫ﺑﺮرﺳﯽ‬ ‫ﺑﺎ‬
‫ﻣﻘﺎﻃﻊ‬ ‫رﺳﻮﺑﯽ‬ ‫ﺑﺎﻓﺖ‬‫ﻣﺠﻤﻮع‬ ‫در‬ ،‫اﺳﮑﻠﺘﯽ‬ ‫ﻏﯿﺮ‬ ‫ﻋﻨﺎﺻﺮ‬ ‫و‬ ‫اﺳﮑﻠﺘﯽ‬ ‫ﻋﻨﺎﺻﺮ‬ ‫ﺷﻨﺎﺳﺎﯾﯽ‬ ‫و‬ ‫ﻣﯿﮑﺮوﺳﮑﻮﭘﯽ‬14‫و‬ ‫رﺧﺴﺎره‬ ‫رﯾﺰ‬4‫رﯾﺰ‬ ‫زﯾﺮ‬
‫رﺧﺴﺎره‬ .‫ﮔﺮدﯾﺪ‬ ‫ﻣﻌﺮﻓﯽ‬ ‫درﯾﺲ‬ ‫ﺑﺮش‬ ‫در‬ ‫آﺳﻤﺎري‬ ‫ﺳﺎزﻧﺪ‬ ‫ﺑﺮاي‬ ‫رﺳﻮﺑﯽ‬ ‫رﺧﺴﺎره‬‫ﺑﻪ‬ ‫ﺳﺎﺣﻞ‬ ‫ﺳﻤﺖ‬ ‫ﺑﻪ‬ ‫ﺑﺎز‬ ‫درﯾﺎي‬ ‫از‬ ‫ﺷﺪه‬ ‫ﺗﻌﯿﯿﻦ‬ ‫ﻫﺎي‬
‫ﻣﯽ‬ ‫داده‬ ‫ﺷﺮح‬ ‫ﺗﺮﺗﯿﺐ‬:‫ﺷﻮﻧﺪ‬
1-‫ﻓﻠﻮﺗﺴﺘﻮن‬-‫ﻧﻮﻣﻮﻟﯿﺘﯿﺪه‬ ‫رودﺳﺘﻮن‬‫ﺑﺎﯾﻮﮐ‬‫ﻼﺳﺖ‬‫دار‬

4. ‫رﯾﺰ‬‫رﺧﺴﺎره‬‫ﻫﺎ‬‫و‬‫ﻣﺪل‬‫رﺳﻮﺑﯽ‬‫ﺳﺎزﻧﺪ‬‫آﺳﻤﺎري‬)‫اﻟﯿﮕﻮﺳﻦ‬(‫در‬‫ﺷﻤﺎل‬‫ﻏﺮب‬‫روﺳﺘﺎي‬‫درﯾﺲ‬...
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rudstone-Bioclastic nummulitidae floatstone-1O
) ‫ﻧﻮﻣﻮﻟﯿﺘﯿﺪه‬ ‫ﺧﺎﻧﻮاده‬ ‫از‬ ‫ﺑﺰرگ‬ ‫ﻣﻨﻔﺬدار‬ ‫ﻓﺮاﻣﯿﻨﯿﻔﺮﻫﺎي‬ ‫رﺧﺴﺎره‬ ‫رﯾﺰ‬ ‫اﯾﻦ‬ ‫اﺻﻠﯽ‬ ‫ﻋﻨﺎﺻﺮ‬ :‫ﺗﻮﺻﯿﻒ‬Nummulites sp.،Operculina
sp.‫و‬Heterostegina sp.‫ﻣﯽ‬ (‫)ﺷﮑﻞ‬ ‫ﺑﺎﺷﺪ‬2-A‫ﺗﺸﮑﯿﻞ‬ .(‫دﻫﻨﺪه‬‫آﻣﻔﯽ‬ ،‫اﻟﻔﯿﺪﯾﻮم‬ ‫ﻓﺮﻋﯽ‬ ‫ﻫﺎي‬،‫ﺳﺘﮋﯾﻨﺎ‬‫ﺗﮑﺴﺘﻮﻻرﯾ‬ ،‫دﻧﺪرﯾﺘﯿﻨﺎ‬،‫ﺪ‬
‫ﮐﻮراﻟﯿﻨﺎﺳﻪ‬ ‫ﻗﺮﻣﺰ‬ ‫ﺟﻠﺒﮏ‬ ‫و‬ ‫اﮐﯿﻨﻮﺋﯿﺪ‬ ،‫ﺑﺮﯾﻮزوﺋﺮ‬ ،‫اﺳﻔﺮوژﯾﭙﺴﯿﻨﺎ‬ ،‫ﻫﺎﭘﻠﻮﻓﺮاﮔﻤﯿﻮم‬ ،‫ﻧﺌﻮروﺗﺎﻟﯿﺎ‬ ،‫ﭘﻼﻧﻮرﺑﻮﻟﯿﻨﺎ‬‫آ‬‫ﻓﺮاواﻧﯽ‬ ‫دﻟﯿﻞ‬ ‫ﺑﻪ‬ .‫ﻫﺴﺘﻨﺪ‬
‫ﺑﺎﯾﻮﮐﻼﺳﺖ‬ ‫اﮐﯿﻨﻮﺋﯿﺪ‬ ‫و‬ ‫ﻧﻮﻣﻮﻟﯿﺘﯿﺪه‬ ‫رودﺳﺘﻮن‬ ‫ـ‬ ‫ﻓﻠﻮﺗﺴﺘﻮن‬ ‫رﺧﺴﺎره‬ ‫رﯾﺰ‬ ‫زﯾﺮ‬ ،‫ﻣﻘﺎﻃﻊ‬ ‫از‬ ‫ﺑﺮﺧﯽ‬ ‫در‬ ‫اﮐﯿﻨﻮﺋﯿﺪ‬‫ﻣﻌ‬ ‫دار‬‫ﻣﯽ‬ ‫ﺮﻓﯽ‬:‫ﮔﺮدد‬
rudstone-Bioclastic nummulitidae echinoids floatstone-1-1O
‫داﻧﻪ‬ ‫اﻧﺪازه‬‫از‬ ‫)ﺑﯿﺸﺘﺮ‬ ‫درﺷﺖ‬ ‫ﺗﺎ‬ ‫رﯾﺰ‬ ‫رﺧﺴﺎره‬ ‫رﯾﺰ‬ ‫اﯾﻦ‬ ‫ﻫﺎي‬2‫ﻣﯿﻠﯽ‬.‫دارﻧﺪ‬ ‫ﺣﻀﻮر‬ ‫ﻣﯿﮑﺮاﯾﺘﯽ‬ ‫ﮐﺮﺑﻨﺎﺗﻪ‬ ‫زﻣﯿﻨﻪ‬ ‫ﯾﮏ‬ ‫در‬ ‫و‬ ‫ﺑﻮده‬ (‫ﻣﺘﺮ‬
‫ﺣﻀﻮر‬ ‫ﻫﻤﭽﻨﯿﻦ‬ ‫و‬ ‫ﻓﺮاﻣﯿﻨﯿﻔﺮﻫﺎ‬ ‫ﭘﻮﺳﺘﻪ‬ ‫در‬ ‫ﺧﺮدﺷﺪﮔﯽ‬ ‫و‬ ‫ﻓﺮﺳﺎﯾﺶ‬ ‫وﺟﻮد‬ ‫ﻋﺪم‬ :‫ﺗﻔﺴﯿﺮ‬‫ﺗ‬ ‫ﺑﺎ‬ ‫ﻧﻮﻣﻮﻟﯿﺘﯿﺪه‬ ‫ﺧﺎﻧﻮاده‬ ‫ﻓﺮاﻣﯿﻨﯿﻔﺮﻫﺎي‬‫ﻨﻮع‬
‫ﺗﻪ‬ ‫از‬ ‫ﺣﺎﮐﯽ‬ ‫رودﺳﺘﻮن‬ ‫ﺗﺎ‬ ‫ﻓﻠﻮﺗﺴﺘﻮن‬ ‫ﺑﺎﻓﺖ‬ ‫در‬ ‫ﺧﻮب‬ ‫ﺷﺪﮔﯽ‬ ‫ﺣﻔﻆ‬ ‫و‬ ‫ﺑﺎﻻ‬‫ﺑﺎ‬ ‫ﺑﺎز‬ ‫درﯾﺎي‬ ‫ﻣﺤﯿﻂ‬ ‫ﯾﮏ‬ ‫در‬ ‫رﺧﺴﺎره‬ ‫رﯾﺰ‬ ‫اﯾﻦ‬ ‫ﻧﺸﺴﺖ‬
‫ﺑﺨﺶ‬ ‫در‬ ‫ﻋﺎدي‬ ‫اﻣﻮاج‬ ‫اﺳﺎس‬ ‫ﺳﻄﺢ‬ ‫زﯾﺮ‬ ‫و‬ ‫ﻣﺘﻮﺳﻂ‬ ‫ﺗﺎ‬ ‫ﮐﻢ‬ ‫اﻧﺮژي‬،‫)ﮔﯿﻞ‬ ‫اﺳﺖ‬ ‫ﻣﯿﺎﻧﯽ‬ ‫رﻣﭗ‬ ‫ﺗﺤﺘﺎﻧﯽ‬ ‫ﻫﺎي‬2000‫رﯾﺰ‬ ‫اﯾﻦ‬ ‫ﻣﺤﺪوده‬ .(
‫از‬ ‫رﺧﺴﺎره‬‫ﺿﺨﺎﻣﺖ‬ ‫ﺗﺎ‬ ‫ﻣﻄﺎﻟﻌﻪ‬ ‫ﺑﺮش‬ ‫ﻗﺎﻋﺪه‬50‫ﻣﯽ‬ ‫ﻣﺘﺮ‬‫ﺟﻨﺲ‬ ‫ﺣﻀﻮر‬ ‫دﻟﯿﻞ‬ ‫ﺑﻪ‬ ‫و‬ ‫ﺑﺎﺷﺪ‬Nummulites sp.‫ﺗﻌﻠﻖ‬ ‫روﭘﻠﯿﻦ‬ ‫زﻣﺎن‬ ‫ﺑﻪ‬
) ‫دارد‬،‫ﻫﻤﮑﺎران‬ ‫و‬ ‫ﻻرﺳﻦ‬2009‫ون‬ ‫؛‬،‫ﻫﻤﮑﺎران‬ ‫و‬ ‫ﺑﻮﺧﻢ‬2010‫ﻣﻨﻄﻘﻪ‬ ‫در‬ ‫آﺳﻤﺎري‬ ‫ﺳﺎزﻧﺪ‬ ‫ﺑﺮاي‬ ‫رﺧﺴﺎره‬ ‫رﯾﺰ‬ ‫اﯾﻦ‬ ‫ﻣﺸﺎﺑﻪ‬ ‫رﺧﺴﺎره‬ .(
‫و‬ ‫)ﺻﺎدﻗﯽ‬ ‫اﺳﺖ‬ ‫ﺷﺪه‬ ‫داده‬ ‫ﻧﺴﺒﺖ‬ ‫ﻣﯿﺎﻧﯽ‬ ‫ﺷﻠﻒ‬ ‫ﺑﻪ‬ ‫ﮐﺎزرون‬،‫ﻫﻤﮑﺎران‬2009.(
2-‫ﺑﺎﯾﻮﮐﻼﺳﺖ‬ ‫ﻧﻮﻣﻮﻟﯿﺘﯿﺪه‬ ‫و‬ ‫ﻟﭙﯿﺪوﺳﯿﮑﻠﯿﻨﯿﺪه‬ ،‫ﻧﺌﻮروﺗﺎﻟﯿﺎ‬ ‫رودﺳﺘﻮن‬‫دار‬
Bioclastic nummulitidae lepidocyclinidae Neorotalia rudstone-2O
‫آﻟﻮﮐﻢ‬ ‫ﻟﭙﯿﺪوﺳﯿﮑﻠﯿﻨﯿﺪه‬ ‫و‬ ‫ﻧﻮﻣﻮﻟﯿﺘﯿﺪه‬ ‫ﺧﺎﻧﻮاده‬ ‫ﻓﺮاﻣﯿﻨﯿﻔﺮﻫﺎي‬ ،‫ﻧﺌﻮروﺗﺎﻟﯿﺎ‬ :‫ﺗﻮﺻﯿﻒ‬‫ﺗﺸﮑ‬ ‫را‬ ‫رﺧﺴﺎره‬ ‫رﯾﺰ‬ ‫اﯾﻦ‬ ‫اﺻﻠﯽ‬ ‫ﻫﺎي‬‫ﻣﯽ‬ ‫ﯿﻞ‬‫دﻫﻨﺪ‬
‫)ﺷﮑﻞ‬2-B‫ﻟﭙﯿﺪوﺳﯿﮑﻠﯿﻨﯿﺪه‬ .(‫ﺷﺎﻣﻞ‬ ‫ﻫﺎ‬Nephrolepidina sp.‫و‬Eulepidina sp.‫ﻣﯽ‬،‫اﻟﻔﯿﺪﯾﻮم‬ ‫ﺷﺎﻣﻞ‬ ‫ﻧﯿﺰ‬ ‫ﻓﺮﻋﯽ‬ ‫ﻋﻨﺎﺻﺮ‬ .‫ﺑﺎﺷﺪ‬
‫آﻣﻔﯽ‬ ،‫ﭘﻼﻧﻮرﺑﻮﻟﯿﻨﺎ‬‫ﮐﻮراﻟﯿﻨﺎﺳﻪ‬ ‫ﻗﺮﻣﺰ‬ ‫ﺟﻠﺒﮏ‬ ‫و‬ ‫ﺳﺘﮋﯾﻨﺎ‬.‫اﺳﺖ‬ ‫آ‬
‫ﭘﺸﺘﯿﺒﺎن‬ ‫داﻧﻪ‬ ‫ﺻﻮرت‬ ‫ﺑﻪ‬ ‫رﺧﺴﺎره‬ ‫رﯾﺰ‬ ‫اﯾﻦ‬ :‫ﺗﻔﺴﯿﺮ‬‫ﺣﻀﻮر‬ ‫دﻟﯿﻞ‬ ‫ﺑﻪ‬ ‫و‬ ‫ﺑﻮده‬ ‫ﻣﯿﮑﺮاﯾﺖ‬ ‫زﻣﯿﻨﻪ‬ ‫در‬‫ﮐ‬ ‫ﻟﭙﯿﺪوﺳﯿﮑﻠﯿﻨﯿﺪﻫﺎي‬ً‫ا‬‫اﮐﺜﺮ‬ ‫ﮐﻪ‬ ‫ﺸﯿﺪه‬
‫از‬2‫ﻣﯿﻠﯽ‬‫ﺑﺰرگ‬ ‫ﻣﺘﺮ‬‫ﻣﯽ‬ ‫ﺗﺮ‬‫ﻣﯽ‬ ‫ﻣﻌﺮﻓﯽ‬ ‫رودﺳﺘﻮن‬ ‫ﻋﻨﻮان‬ ‫ﺑﻪ‬ ‫آن‬ ‫ﺑﺎﻓﺖ‬ ،‫ﺑﺎﺷﻨﺪ‬،‫ﮐﻠﻮان‬ ‫و‬ ‫)اﻣﺒﺮي‬ ‫ﺷﻮد‬1971،‫راﯾﺖ‬ ‫؛‬1992‫ﻫﻤﺎﻧﻨﺪ‬ .(
‫ﺗﻪ‬ ‫ﮐﻨﻨﺪه‬ ‫ﺑﯿﺎن‬ ‫ﻧﯿﺰ‬ ‫رﺧﺴﺎره‬ ‫رﯾﺰ‬ ‫اﯾﻦ‬ ،‫ﻗﺒﻞ‬ ‫رﺧﺴﺎره‬ ‫رﯾﺰ‬‫ﺳﻄﺢ‬ ‫زﯾﺮ‬ ‫و‬ ‫ﻣﺘﻮﺳﻂ‬ ‫اﻧﺮژي‬ ‫ﺑﺎ‬ ‫ﺑﺎز‬ ‫درﯾﺎي‬ ‫ﻣﺤﯿﻂ‬ ‫ﯾﮏ‬ ‫در‬ ‫رﺳﻮﺑﺎت‬ ‫ﻧﺸﺴﺖ‬
‫اﺳﺎس‬‫ﺑﺨﺶ‬ ‫در‬ ‫ﻋﺎدي‬ ‫اﻣﻮاج‬‫ﻣﯽ‬ ‫ﻣﯿﺎﻧﯽ‬ ‫رﻣﭗ‬ ‫ﺗﺤﺘﺎﻧﯽ‬ ‫ﻫﺎي‬،‫)ﮔﯿﻞ‬ ‫ﺑﺎﺷﺪ‬2000‫ﺿﺨﺎﻣﺖ‬ ‫از‬ ‫رﺧﺴﺎره‬ ‫رﯾﺰ‬ ‫اﯾﻦ‬ .(68-63‫ﺑﺮش‬ ‫ﻣﺘﺮي‬
‫روﭘﻠﯿﻦ‬ ‫ﻣﺮز‬ ‫ﺣﺪ‬ ‫در‬ ‫ﻣﻄﺎﻟﻌﻪ‬‫ـ‬‫ﺗﻪ‬ ‫ﺷﺎﺗﯿﻦ‬‫رﺧﺴﺎره‬ .‫اﺳﺖ‬ ‫ﺷﺪه‬ ‫ﻧﺸﯿﻦ‬‫ﺷﻤﺎل‬ ‫در‬ ‫رﺧﺴﺎره‬ ‫رﯾﺰ‬ ‫اﯾﻦ‬ ‫ﻣﺸﺎﺑﻪ‬ ‫ﻫﺎي‬‫زاﮔﺮس‬ ‫ﺣﻮﺿﻪ‬ ‫ﻏﺮب‬
‫)وزﯾﺮي‬،‫ﻫﻤﮑﺎران‬ ‫و‬ ‫ﻣﻘﺪم‬2010‫)ﺷﺐ‬ ‫ﮔﭽﺴﺎران‬ ‫در‬ ‫و‬ (‫اﻓﺮوز‬،‫ﻫﻤﮑﺎران‬ ‫و‬2015.‫اﺳﺖ‬ ‫ﺷﺪه‬ ‫ﻣﻄﺎﻟﻌﻪ‬ (
3-‫ﭘﮑﺴﺘﻮن‬-‫ﺑﺎﯾﻮﮐﻼﺳﺖ‬ ‫ﻧﺌﻮروﺗﺎﻟﯿﺎ‬ ‫و‬ ‫ﻧﻮﻣﻮﻟﯿﺘﯿﺪه‬ ‫رودﺳﺘﻮن‬‫دار‬
rudstone-Bioclastic Neorotalia nummulitidae packstone-3O
‫آﻟﻮﮐﻢ‬ :‫ﺗﻮﺻﯿﻒ‬‫ﻣﯽ‬ ‫ﻧﻮﻣﻮﻟﯿﺘﯿﺪه‬ ‫ﺧﺎﻧﻮاده‬ ‫ﻓﺮاﻣﯿﻨﯿﻔﺮﻫﺎي‬ ‫و‬ ‫ﻧﺌﻮروﺗﺎﻟﯿﺎ‬ ‫ﺷﺎﻣﻞ‬ ‫اﺻﻠﯽ‬ ‫ﻫﺎي‬‫)ﺷﮑﻞ‬ ‫ﺑﺎﺷﺪ‬2-C‫ﭘﻼ‬ ،‫اﻟﻔﯿﺪﯾﻮم‬ .(،‫ﻧﻮرﺑﻮﻟﯿﻨﺎ‬
‫ﮐﻮراﻟﯿﻨﺎﺳﻪ‬ ‫ﻗﺮﻣﺰ‬ ‫ﺟﻠﺒﮏ‬ ‫و‬ ‫ﺑﺮﯾﻮزوﺋﺮ‬ ،‫اﮐﯿﻨﻮﺋﯿﺪ‬ ،‫دﻧﺪرﯾﺘﯿﻨﺎ‬ ،‫ﺗﮑﺴﺘﻮﻻرﯾﺪ‬‫داﻧﻪ‬ ‫آ‬‫ﻣﯽ‬ ‫رﺧﺴﺎره‬ ‫رﯾﺰ‬ ‫اﯾﻦ‬ ‫ﻓﺮﻋﯽ‬ ‫ﻫﺎي‬‫ﺑﺎﺷ‬‫ﻗﺮﻣﺰ‬ ‫ﺟﻠﺒﮏ‬ .‫ﻨﺪ‬

5. ‫رﯾﺰ‬‫رﺧﺴﺎره‬‫ﻫﺎ‬‫و‬‫ﻣﺪل‬‫رﺳﻮﺑﯽ‬‫ﺳﺎزﻧﺪ‬‫آﺳﻤﺎري‬)‫اﻟﯿﮕﻮﺳﻦ‬(‫در‬‫ﺷﻤﺎل‬‫ﻏﺮب‬‫روﺳﺘﺎي‬‫درﯾﺲ‬...
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‫ﺷﺎﻣﻞ‬Lithophyllum sp.‫و‬Subterranophyllum thomasi‫آن‬ ‫اﻓﺰاﯾﺶ‬ ‫دﻟﯿﻞ‬ ‫ﺑﻪ‬ ‫ﻣﻘﺎﻃﻊ‬ ‫از‬ ‫ﺑﺮﺧﯽ‬ ‫در‬ ‫ﮐﻪ‬ ‫اﺳﺖ‬‫رﯾﺰ‬ ‫زﯾﺮ‬ ،‫ﻫﺎ‬
‫ﭘﮑﺴﺘﻮن‬ ‫رﺧﺴﺎره‬-‫رودﺳﺘﻮن‬‫ﮐﻮراﻟﯿﻨﺎﺳﻪ‬ ‫و‬ ‫ﻧﻮﻣﻮﻟﯿﺘﯿﺪه‬ ،‫ﻧﺌﻮروﺗﺎﻟﯿﺎ‬‫ﺑﺎﯾﻮﮐﻼﺳﺖ‬ ‫آ‬‫ﻣﯽ‬ ‫ﻣﻌﺮﻓﯽ‬ ‫دار‬:‫ﮔﺮدد‬
rudstone-Bioclastic Neorotalia nummulitidae corallinacean packstone-1-3O
‫داﻧﻪ‬ ‫ﺣﻀﻮر‬ ‫ﻋﻠﺖ‬ ‫ﺑﻪ‬ ‫رﺧﺴﺎره‬ ‫رﯾﺰ‬ ‫اﯾﻦ‬ ‫ﺑﺎﻓﺖ‬ :‫ﺗﻔﺴـﯿﺮ‬‫اﻧﺪازه‬ ‫)ﺑﺎ‬ ‫اﺳﮑﻠﺘﯽ‬ ‫ﻫﺎي‬،‫ﻣﯿﮑﺮاﯾﺖ‬ ‫زﻣﯿﻨﻪ‬ ‫در‬ ‫ﻏﺎﻟﺐ‬ ‫ﺻﻮرت‬ ‫ﺑﻪ‬ (‫ﻣﺘﻔﺎوت‬ ‫ﻫﺎي‬
‫ﺑﻪ‬‫ﻣﯽ‬ ‫ﻣﻌﺮﻓﯽ‬ ‫رودﺳــﺘﻮن‬ ‫ﯾﺎ‬ ‫ﭘﮑﺴــﺘﻮن‬ ‫ﺻــﻮرت‬‫ﻣﯽ‬ ‫ﻣﺤﯿﻂ‬ ‫زﯾﺎد‬ ‫ﺗﺎ‬ ‫ﻣﺘﻮﺳــﻂ‬ ‫اﻧﺮژي‬ ‫از‬ ‫ﺣﺎﮐﯽ‬ ‫ﮐﻪ‬ ‫ﺷــﻮد‬‫ﺣﻀــﻮر‬ ‫ﻋﻠﺖ‬ ‫ﺑﻪ‬ .‫ﺑﺎﺷــﺪ‬
‫ﺑﻪ‬ ‫ﻫﯿﺎﻟﯿﻦ‬ ‫آﻫﮏ‬ ‫دﯾﻮاره‬ ‫ﺑﺎ‬ ‫درﯾﺎﯾﯽ‬ ‫ﻧﺮﻣﺎل‬ ‫ﺷﻮري‬ ‫ﻣﻌﺮف‬ ‫ﻓﺮاﻣﯿﻨﯿﻔﺮﻫﺎي‬‫ﺑﻪ‬ ‫ﻣﺘﻌﻠﻖ‬ ‫رﺧﺴﺎره‬ ‫رﯾﺰ‬ ‫اﯾﻦ‬ ،‫ﺷﮑﻞ‬ ‫ﻋﺪﺳﯽ‬ ‫ﺗﺎ‬ ‫ﮐﺸﯿﺪه‬ ‫ﺻﻮرت‬
‫ﻣﯽ‬ ‫ﻋﺎدي‬ ‫اﻣﻮاج‬ ‫اﺳـﺎس‬ ‫ﺳـﻄﺢ‬ ‫زﯾﺮ‬ ‫در‬ ‫ﺑﺎز‬ ‫درﯾﺎي‬ ‫ﻋﻤﻖ‬ ‫ﮐﻢ‬ ‫ﺑﺨﺶ‬‫ﺑﺎﺷﺪ‬)Middle ramp،‫)ﮔﯿﻞ‬ (2000‫ﻧﯿﺰ‬ ‫رﺧﺴﺎره‬ ‫رﯾﺰ‬ ‫اﯾﻦ‬ .(
‫ﺷﻤﺎره‬ ‫رﺧﺴﺎره‬ ‫رﯾﺰ‬ ‫ﻫﻤﺎﻧﻨﺪ‬1‫ﮔﻮﻧﻪ‬ ‫ﺣﻀﻮر‬ ‫دﻟﯿﻞ‬ ‫ﺑﻪ‬ ،‫ﺟﻨﺲ‬ ‫ﻫﺎي‬Nummulites sp.‫ﻣﯽ‬ ‫ﻣﺤﺪود‬ ‫روﭘﻠﯿﻦ‬ ‫زﻣﺎن‬ ‫ﺑﻪ‬) ‫ﺷﻮد‬‫و‬ ‫ﻻرﺳﻦ‬
،‫ﻫﻤﮑﺎران‬2009‫ون‬ ‫؛‬،‫ﻫﻤﮑﺎران‬ ‫و‬ ‫ﺑﻮﺧﻢ‬2010.(
4-‫ﺑﺎﯾﻮﮐﻼﺳﺖ‬ ‫ﻟﭙﯿﺪوﺳﯿﮑﻠﯿﻨﯿﺪ‬ ‫و‬ ‫ﻧﺌﻮروﺗﺎﻟﯿﺎ‬ ‫ﭘﮑﺴﺘﻮن‬‫دار‬
ioclastic Neorotalia lepidocyclinidae packstoneB-4O
:‫ﺗﻮﺻﯿﻒ‬‫آﻟﻮﮐﻢ‬ ‫ﻋﻨﻮان‬ ‫ﺑﻪ‬ ‫ﻧﺌﻮروﺗﺎﻟﯿﺎ‬ ‫و‬ ‫ﮐﻮﭼﮏ‬ ‫ﺷﮑﻞ‬ ‫ﻋﺪﺳﯽ‬ ‫ﻟﭙﯿﺪوﺳﯿﮑﻠﯿﻨﺎﻫﺎي‬‫آﻣﻔﯽ‬ ،‫اﻟﻔﯿﺪﯾﻮم‬ ،‫ﺗﮑﺴﺘﻮﻻرﯾﺪ‬ ‫و‬ ‫ﻏﺎﻟﺐ‬ ‫ﻫﺎي‬،‫ﺳﺘﮋﯾﻨﺎ‬
‫ﮐﻮراﻟﯿﻨﺎﺳﻪ‬ ‫ﻗﺮﻣﺰ‬ ‫ﺟﻠﺒﮏ‬ ‫و‬ ‫اﮐﯿﻨﻮﺋﯿﺪ‬ ،‫اﭘﺮﮐﻮﻟﯿﻨﺎ‬ ،‫ﻫﺘﺮوﺳﺘﮋﯾﻨﺎ‬ ،‫ﭘﻼﻧﻮرﺑﻮﻟﯿﻨﺎ‬‫رﺧﺴﺎره‬ ‫رﯾﺰ‬ ‫اﯾﻦ‬ ‫ﻓﺮﻋﯽ‬ ‫ﻋﻨﺎﺻﺮ‬ ‫آ‬‫ﻣﺤﺴ‬‫ﻣﯽ‬ ‫ﻮب‬‫ﺷﻮﻧﺪ‬‫)ﺷﮑﻞ‬
2-D(‫ﮐﻮراﻟﯿﻨﺎﺳﻪ‬ ‫و‬ ‫ﻟﭙﯿﺪوﺳﯿﮑﻠﯿﻨﯿﺪ‬ ،‫ﻧﺌﻮروﺗﺎﻟﯿﺎ‬ ‫ﭘﮑﺴﺘﻮن‬ ‫رﺧﺴﺎره‬ ‫رﯾﺰ‬ ‫زﯾﺮ‬ ،‫ﻣﯿﮑﺮوﻓﺎﺳﯿﺲ‬ ‫اﯾﻦ‬ ‫در‬ ‫ﻗﺮﻣﺰ‬ ‫ﺟﻠﺒﮏ‬ ‫اﻓﺰاﯾﺶ‬ ‫ﺑﺎ‬ .‫آ‬
‫ﺑﺎﯾﻮﮐﻼﺳﺖ‬‫ﻣﯽ‬ ‫ﻣﻌﺮﻓﯽ‬ ‫دار‬:‫ﺷﻮد‬
Bioclastic Neorotalia lepidocyclinidae corallinacean packstone-1-4O
‫اﺳﮑﻠﺘﯽ‬ ‫ﻋﻨﺎﺻﺮ‬ ‫رﺧﺴﺎره‬ ‫رﯾﺰ‬ ‫اﯾﻦ‬ ‫در‬‫ﮐﻮﭼﮏ‬ ً‫ﺎ‬‫)ﻏﺎﻟﺒ‬‫از‬ ‫ﺗﺮ‬2‫ﻣﯿﻠﯽ‬.‫دارﻧﺪ‬ ‫ﺣﻀﻮر‬ ‫ﮔﻠﯽ‬ ‫زﻣﯿﻨﻪ‬ ‫در‬ ‫ﭘﺸﺘﯿﺒﺎن‬ ‫داﻧﻪ‬ ‫ﺻﻮرت‬ ‫ﺑﻪ‬ (‫ﻣﺘﺮ‬
:‫ﺗﻔﺴﯿﺮ‬‫رﺳﻮﺑﯽ‬ ‫ﻣﺤﯿﻂ‬ ‫زﯾﺎد‬ ‫اﻧﺮژي‬ ‫از‬ ‫ﺣﺎﮐﯽ‬ ‫رﺧﺴﺎره‬ ‫رﯾﺰ‬ ‫اﯾﻦ‬ ‫ﺑﻮدن‬ ‫ﭘﺸﺘﯿﺒﺎن‬ ‫داﻧﻪ‬‫ﻣﯽ‬‫ﻟﭙﯿﺪوﺳﯿﮑﻠﯿﻨ‬ ‫ﺣﺎوي‬ ‫رﺳﻮﺑﺎت‬ .‫ﺑﺎﺷﺪ‬‫ﯿﺪه‬‫ﻫﺎي‬
‫ﻧﻤﻮﻧﻪ‬ ‫ﺣﺎوي‬ ‫رﺳﻮﺑﺎت‬ ‫ﺑﻪ‬ ‫ﻧﺴﺒﺖ‬ ‫ﮔﺮد‬ ‫و‬ ‫ﺷﮑﻞ‬ ‫ﻋﺪﺳﯽ‬‫ﮐﻢ‬ ‫ﻣﺤﯿﻂ‬ ‫ﮐﺸﯿﺪه‬ ‫و‬ ‫ﺑﺰرگ‬ ‫ﻫﺎي‬‫ﻋﻤ‬‫ﻖ‬‫ﻣﯽ‬ ‫ﻧﺸﺎن‬ ‫را‬ ‫ﺗﺮي‬‫و‬ ‫)ﺑﺎراﺗﻠﻮ‬ ‫دﻫﻨﺪ‬
،‫ﻫﻤﮑﺎران‬2007‫ﺗﺎﮐﺴﻮن‬ ‫اﯾﻦ‬ ‫وﺟﻮد‬ .(‫ﻣﯽ‬ ‫درﯾﺎﯾﯽ‬ ‫ﻧﺮﻣﺎل‬ ‫ﺷﻮري‬ ‫ﻣﻌﺮف‬ ‫)ﮐﻪ‬‫ﻣﯽ‬ ‫ﺳﺒﺐ‬ ،‫زﯾﺎد‬ ‫ﺗﺤﺪب‬ ‫ﺑﺎ‬ (‫ﺑﺎﺷﺪ‬‫رﯾﺰ‬ ‫اﯾﻦ‬ ‫ﮐﻪ‬ ‫ﺷﻮد‬
‫ﮐﻢ‬ ‫ﺑﺨﺶ‬ ‫ﺑﻪ‬ ‫را‬ ‫رﺧﺴﺎره‬) ‫ﺑﺎز‬ ‫درﯾﺎي‬ ‫ﻋﻤﻖ‬Proximal middle ramp،‫)ﭘﻮﻣﺎر‬ ‫دﻫﯿﻢ‬ ‫ﻧﺴﺒﺖ‬ ‫ﻣﯿﺎﻧﯽ‬ ‫رﻣﭗ‬ ‫در‬ (2001.(‫رﺧﺴﺎره‬ ‫رﯾﺰ‬
،‫ﻫﻤﮑﺎران‬ ‫و‬ ‫)ﺻﺎدﻗﯽ‬ ‫اﺳﺖ‬ ‫ﺷﺪه‬ ‫ﺷﻨﺎﺳﺎﯾﯽ‬ ‫ﻧﯿﺰ‬ ‫زاﮔﺮس‬ ‫ﺣﻮﺿﻪ‬ ‫در‬ ‫ﻓﺎرس‬ ‫ﻣﻨﻄﻘﻪ‬ ‫در‬ ‫ﻣﯿﮑﺮوﻓﺎﺳﯿﺲ‬ ‫اﯾﻦ‬ ‫ﻣﺸﺎﺑﻪ‬2010.(
5-‫ﮐﻮراﻟﯿﻨﺎﺳﻪ‬ ‫ﭘﮑﺴﺘﻮن‬‫ﺑﺎﯾﻮﮐﻼﺳﺖ‬ ‫ﻧﺌﻮروﺗﺎﻟﯿﺎ‬ ‫و‬ ‫آ‬‫دار‬
Bioclastic Neorotalia corallinacean packstone-5O
:‫ﺗﻮﺻﯿﻒ‬‫ﮐﻮر‬ ‫ﻗﺮﻣﺰ‬ ‫ﺟﻠﺒﮏ‬ ‫ﻫﻤﺮاﻫﯽ‬ ‫ﻋﻠﺖ‬ ‫ﺑﻪ‬ ‫رﺧﺴﺎره‬ ‫رﯾﺰ‬ ‫اﯾﻦ‬‫اﻟﯿﻨﺎﺳﻪ‬‫داﻧﻪ‬ ‫ﻋﻨﻮان‬ ‫ﺑﻪ‬ ‫ﻧﺌﻮروﺗﺎﻟﯿﺎ‬ ‫و‬ ‫آ‬‫ﻣﯽ‬ ‫ﻣﻌﺮﻓﯽ‬ ‫اﺻﻠﯽ‬ ‫ﻫﺎي‬‫ﺷ‬‫ﻮد‬
‫)ﺷﮑﻞ‬2-E(‫آﻣﻔﯽ‬ ،‫ﻣﯿﻠﯿﻮﻟﯿﺪ‬ ،‫ﭘﻼﻧﻮرﺑﻮﻟﯿﻨﺎ‬ ‫ﺷﺎﻣﻞ‬ ‫ﻓﺮﻋﯽ‬ ‫ﻋﻨﺎﺻﺮ‬ .‫ﻣﯽ‬ ‫اﮐﯿﻨﻮﺋﯿﺪ‬ ‫و‬ ‫ﺑﺮﯾﻮزوﺋﺮ‬ ،‫اﻟﻔﯿﺪﯾﻮم‬ ،‫ﻫﺘﺮوﺳﺘﮋﯾﻨﺎ‬ ،‫ﺳﺘﮋﯾﻨﺎ‬‫ﺑ‬.‫ﺎﺷﻨﺪ‬
‫ﺣﻀﻮر‬ :‫ﺗﻔﺴﯿﺮ‬‫ﮐﻮراﻟﯿﻨﺎﺳﻪ‬ ‫و‬ ‫ﻧﺌﻮروﺗﺎﻟﯿﺎ‬‫زﻣﯿﻨﻪ‬ ‫در‬ ‫ﻓﺮاوان‬ ‫ﻣﻘﺪار‬ ‫ﺑﻪ‬ ‫ﺷﺪه‬ ‫ﺧﺮد‬ ‫ﺻﻮرت‬ ‫ﺑﻪ‬ ‫آ‬‫داﻧﻪ‬ ‫ﺻﻮرت‬ ‫ﺑﻪ‬ ‫ﮔﻠﯽ‬‫ﭘﺸﺘﯿ‬‫ﮐﻨﻨﺪه‬ ‫ﺑﯿﺎن‬ ‫ﺒﺎن‬
‫رﻣﭗ‬ ‫در‬ ‫ﺑﺎز‬ ‫درﯾﺎي‬ ‫ﻋﻤﻖ‬ ‫ﮐﻢ‬ ‫ﺑﺨﺶ‬ ‫ﺑﻪ‬ ‫ﻣﺮﺑﻮط‬ ‫رﺧﺴﺎره‬ ‫رﯾﺰ‬ ‫اﯾﻦ‬ .‫اﺳﺖ‬ ‫آزاد‬ ‫آب‬ ‫ﭼﺮﺧﺶ‬ ‫ﺑﺎ‬ ‫رﺳﻮﺑﯽ‬ ‫ﻣﺤﯿﻂ‬ ‫زﯾﺎد‬ ‫ﺗﺎ‬ ‫ﻣﺘﻮﺳﻂ‬ ‫اﻧﺮژي‬
‫ﻣﯽ‬ ‫ﮔﺮﻓﺘﻪ‬ ‫ﻧﻈﺮ‬ ‫در‬ ‫ﺑﺎﯾﻮﮐﻼﺳﺘﯽ‬ ‫ﺳﺪ‬ ‫ﺳﻤﺖ‬ ‫ﺑﻪ‬ ‫ﻣﯿﺎﻧﯽ‬،‫)ﭘﻮﻣﺎر‬ ‫ﺷﻮد‬2001.(

6. ‫رﯾﺰ‬‫رﺧﺴﺎره‬‫ﻫﺎ‬‫و‬‫ﻣﺪل‬‫رﺳﻮﺑﯽ‬‫ﺳﺎزﻧﺪ‬‫آﺳﻤﺎري‬)‫اﻟﯿﮕﻮﺳﻦ‬(‫در‬‫ﺷﻤﺎل‬‫ﻏﺮب‬‫روﺳﺘﺎي‬‫درﯾﺲ‬...
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6-‫ﭘﮑﺴﺘﻮن‬-‫ﮐﻮراﻟﯿﻨﺎﺳﻪ‬ ،‫ﻧﺌﻮروﺗﺎﻟﯿﺎ‬ ‫رودﺳﺘﻮن‬‫ﻣﺮﺟﺎن‬ ‫و‬ ‫آ‬‫ﺑﺎﯾﻮﮐﻼﺳﺖ‬‫دار‬
rudstone-Bioclastic coral corallinacean Neorotalia packstone-6O
‫داﻧﻪ‬ :‫ﺗﻮﺻﯿﻒ‬‫ﮐﻮراﻟﯿﻨﺎﺳﻪ‬ ‫ﻗﺮﻣﺰ‬ ‫ﺟﻠﺒﮏ‬ ،‫ﻧﺌﻮروﺗﺎﻟﯿﺎ‬ ‫رﺧﺴﺎره‬ ‫رﯾﺰ‬ ‫اﯾﻦ‬ ‫اﺻﻠﯽ‬ ‫ﻫﺎي‬‫واﻟﻮوﻟﯿﻨﯿ‬ ،‫رﺋﻮﺳﻼ‬ ‫ﺷﺎﻣﻞ‬ ‫ﻓﺮﻋﯽ‬ ‫ﻋﻨﺎﺻﺮ‬ ‫و‬ ‫ﻣﺮﺟﺎن‬ ،‫آ‬،‫ﺪ‬
‫ﻣﯽ‬ ‫ﺑﺮﯾﻮزوﺋﺮ‬ ‫و‬ ‫اﮐﯿﻨﻮﺋﯿﺪ‬ ،‫ﻣﯿﻠﯿﻮﻟﯿﺪ‬‫رﺧﺴﺎره‬ ‫رﯾﺰ‬ ‫اﯾﻦ‬ ‫در‬ .‫ﺑﺎﺷﺪ‬‫آﻟﻮﮐﻢ‬‫ﺑﻪ‬ ‫ﻫﺎ‬‫ﻣﯿﮑﺮاﯾﺖ‬ ‫زﻣﯿﻨﻪ‬ ‫در‬ ‫ﭘﺸﺘﯿﺒﺎن‬ ‫داﻧﻪ‬ ‫ﺻﻮرت‬‫ﺣ‬‫دارﻧﺪ‬ ‫ﻀﻮر‬
‫)ﺷﮑﻞ‬2-F.(
:‫ﺗﻔﺴﯿﺮ‬‫ﺧﺮده‬ ‫ﺣﻀﻮر‬ ‫دﻟﯿﻞ‬ ‫ﺑﻪ‬‫از‬ ‫ﺑﯿﺶ‬ ‫اﻧﺪازه‬ ‫ﺑﺎ‬ ‫ﻣﺮﺟﺎن‬ ‫ﻫﺎي‬2‫ﻣﯿﻠﯽ‬‫ﻣﻌﺮﻓﯽ‬ ‫رﺧﺴﺎره‬ ‫رﯾﺰ‬ ‫اﯾﻦ‬ ‫ﺑﺮاي‬ ‫رودﺳﺘﻮن‬ ‫ﺗﺎ‬ ‫ﭘﮑﺴﺘﻮن‬ ‫ﺑﺎﻓﺖ‬ ‫ﻣﺘﺮ‬
‫ﻣﯽ‬) ‫ﺷﻮد‬،‫ﮐﻠﻮان‬ ‫و‬ ‫اﻣﺒﺮي‬1971،‫راﯾﺖ‬ ‫؛‬1992‫ﺟﻠﺒﮏ‬ ‫ﻗﻄﻌﺎت‬ .(‫ﮐﻮراﻟﯿﻨﺎﺳﻪ‬ ‫ﻗﺮﻣﺰ‬ ‫ﻫﺎي‬‫آ‬‫ﺑﯿﻮﮐﻼﺳﺖ‬ ‫ﺳﺎﯾﺮ‬ ‫و‬‫و‬ ‫ﺷﺪه‬ ‫ﺧﺮد‬ ‫ﻫﺎي‬
‫ﻣﯽ‬ ‫ﻣﺘﻤﺎﯾﺰ‬ ‫رﯾﻔﯽ‬ ‫رﺧﺴﺎره‬ ‫از‬ ‫را‬ ‫رﺧﺴﺎره‬ ‫رﯾﺰ‬ ‫اﯾﻦ‬ ،‫ﺑﺎﻧﺪﺳﺘﻮﻧﯽ‬ ‫ﺳﺎﺧﺘﺎر‬ ‫ﻋﺪم‬ ‫ﻫﻤﭽﻨﯿﻦ‬‫)رﯾﻒ‬ ‫ﺑﺮﺟﺎ‬ ‫ﻓﺎﺑﺮﯾﮏ‬ ‫وﺟﻮد‬ ‫ﻋﺪم‬ ‫ﻫﻤﭽﻨﯿﻦ‬ .‫ﮐﻨﺪ‬
‫ﮐﻮراﻟﯿﻨﺎﺳﻪ‬ ‫ﺣﻀﻮر‬ ‫و‬ (‫ﻣﺮﺟﺎﻧﯽ‬‫داﻧﻪ‬ ‫ﺑﺎﻓﺖ‬ ‫ﯾﮏ‬ ‫در‬ ‫ﻣﺮﺟﺎن‬ ‫و‬ ‫آ‬‫ﻣﯽ‬ ‫رﺳﻮﺑﯽ‬ ‫ﻣﺤﯿﻂ‬ ‫در‬ ‫ﻧﻮر‬ ‫و‬ ‫زﯾﺎد‬ ‫اﻧﺮژي‬ ‫از‬ ‫ﺣﺎﮐﯽ‬ ‫ﭘﺸﺘﯿﺒﺎن‬‫ﺑ‬.‫ﺎﺷﺪ‬
‫ﮐﻢ‬ ‫در‬ ‫رﺧﺴﺎره‬ ‫رﯾﺰ‬ ‫اﯾﻦ‬ ‫ﺑﻨﺎﺑﺮاﯾﻦ‬‫ﻋﻤﻖ‬،‫)وﯾﻠﺴﻮن‬ ‫اﺳﺖ‬ ‫ﺷﺪه‬ ‫ﺗﺸﮑﯿﻞ‬ ‫ﺑﺎﯾﻮﮐﻼﺳﺘﯽ‬ ‫ﺳﺪ‬ ‫ﺳﻤﺖ‬ ‫ﺑﻪ‬ ‫ﺑﺎز‬ ‫درﯾﺎي‬ ‫ﺑﺨﺶ‬ ‫ﺗﺮﯾﻦ‬1975.(
‫)ﺷﺐ‬ ‫اﺳﺖ‬ ‫ﺷﺪه‬ ‫ﮔﺰارش‬ ‫ﻧﯿﺰ‬ ‫ﮔﭽﺴﺎران‬ ‫ﻧﺎﺣﯿﻪ‬ ‫در‬ ‫رﺧﺴﺎره‬ ‫رﯾﺰ‬ ‫اﯾﻦ‬ ‫ﻣﺸﺎﺑﻪ‬،‫ﻫﻤﮑﺎران‬ ‫و‬ ‫اﻓﺮوز‬2015.(
7-‫ﭘﮑﺴﺘﻮن‬-‫ﮐﻮراﻟﯿﻨﺎﺳﻪ‬ ،‫اﮐﯿﻨﻮﺋﯿﺪ‬ ‫ﮔﺮﯾﻨﺴﺘﻮن‬‫ﻧﺌﻮروﺗﺎﻟﯿﺎ‬ ‫و‬ ‫آ‬
Sh- Neorotalia corallinacean echinoids packstone - grainstone
‫ﮐﻮراﻟﯿﻨﺎﺳﻪ‬ ‫ﻗﺮﻣﺰ‬ ‫ﺟﻠﺒﮏ‬ ،‫ﻧﺌﻮروﺗﺎﻟﯿﺎ‬ ‫ﺷﺎﻣﻞ‬ ‫رﺧﺴﺎره‬ ‫رﯾﺰ‬ ‫اﯾﻦ‬ ‫اﺻﻠﯽ‬ ‫ﻋﻨﺎﺻﺮ‬ :‫ﺗﻮﺻﯿﻒ‬‫ﺧﺮده‬ ‫و‬ ‫آ‬‫ﻣﯽ‬ ‫ﺧﺎرﭘﻮﺳﺘﺎن‬ ‫ﻫﺎي‬‫ﺑﺎﺷﺪ‬‫رﯾﺰ‬ ‫اﯾﻦ‬ .
‫ﻣﯽ‬ ‫ﻣﺸﺎﻫﺪه‬ ‫ﮔﻠﯽ‬ ‫زﻣﯿﻨﻪ‬ ‫ﺑﺎ‬ ‫ﻣﻘﺎﻃﻊ‬ ‫از‬ ‫ﺑﺮﺧﯽ‬ ‫در‬ ‫و‬ ‫ﺳﯿﻤﺎن‬ ‫زﻣﯿﻨﻪ‬ ‫ﺑﺎ‬ ‫ﭘﺸﺘﯿﺒﺎن‬ ‫داﻧﻪ‬ ‫ﻓﺎﺑﺮﯾﮏ‬ ‫ﺑﺎ‬ ‫رﺧﺴﺎره‬) ‫ﺷﻮد‬‫ﺷﮑﻞ‬2-G.(
:‫ﺗﻔﺴﯿﺮ‬‫آﻟﻮﮐﻢ‬ ‫ﺧﻮب‬ ‫ﺟﻮرﺷﺪﮔﯽ‬ ‫و‬ ‫ﮐﻢ‬ ‫ﺗﻨﻮع‬ ،‫ﭘﺸﺘﯿﺒﺎن‬ ‫داﻧﻪ‬ ‫ﺑﺎﻓﺖ‬‫ﺗﻪ‬ ‫از‬ ‫ﺣﺎﮐﯽ‬ ‫ﻫﺎ‬‫ﺳﺪ‬ ‫ﻣﺤﯿﻂ‬ ‫ﯾﮏ‬ ‫در‬ ‫رﺧﺴﺎره‬ ‫رﯾﺰ‬ ‫اﯾﻦ‬ ‫ﻧﺸﺴﺖ‬
،‫)ﻓﻠﻮﮔﻞ‬ ‫اﺳﺖ‬ ‫ﺑﺎﻻ‬ ً‫ﺎ‬‫ﻧﺴﺒﺘ‬ ‫اﻧﺮژي‬ ‫ﺑﺎ‬ ‫ﺑﺎﯾﻮﮐﻼﺳﺘﯽ‬2010‫و‬ ‫)ﺻﺎدﻗﯽ‬ ‫اﺳﺖ‬ ‫ﺷﺪه‬ ‫ﮔﺰارش‬ ‫ﻧﯿﺰ‬ ‫ﻓﺎرس‬ ‫زون‬ ‫از‬ ‫رﺧﺴﺎره‬ ‫رﯾﺰ‬ ‫اﯾﻦ‬ ‫ﻣﺸﺎﺑﻪ‬ .(
،‫ﻫﻤﮑﺎران‬2010.(
8-‫ﻓﻠﻮﺗﺴﺘﻮن‬-‫روزن‬ ‫ﺣﺎوي‬ ‫ﻣﺮﺟﺎن‬ ‫رودﺳﺘﻮن‬‫ﮐﻒ‬ ‫داران‬‫زي‬
rudstone-Coral benthic foraminifera floatstone-1L
:‫ﺗﻮﺻﯿﻒ‬‫روزن‬ ‫ﻫﻤﺮاه‬ ‫ﺑﻪ‬ ‫ﻣﺮﺟﺎن‬‫ﮐﻒ‬ ‫داران‬،‫آﺳﺘﺮوﺗﺮﯾﻠﯿﻨﺎ‬ ،‫ﻣﯿﻠﯿﻮﻟﯿﺪ‬ ،‫دﯾﺴﮑﻮرﺑﯿﺲ‬ ،‫رﺋﻮﺳﻼ‬ ،‫واﻟﻮوﻟﯿﻨﯿﺪ‬ ،‫ﭘﻨﺮوﭘﻠﯿﺲ‬ ‫ﻗﺒﯿﻞ‬ ‫از‬ ‫زي‬
‫آﻟﻮﮐﻢ‬ ‫ﮐﻮﭼﮏ‬ ‫روﺗﺎﻟﯿﺪﻫﺎي‬ ‫و‬ ‫ﻫﺎﭘﻠﻮﻓﺮاﮔﻤﯿﻮم‬‫رﯾﺰ‬ ‫اﯾﻦ‬ ‫ﻫﺎي‬‫ﻣﯽ‬ ‫ﻣﺤﺴﻮب‬ ‫رﺧﺴﺎره‬‫ﺧﺮده‬ ،‫ﻣﯿﮑﺮاﯾﺖ‬ .‫ﺷﻮﻧﺪ‬‫ﺟﻠﺒﮏ‬ ‫و‬ ‫اﺳﮑﻠﺘﯽ‬ ‫ﻫﺎي‬
‫ﮐﻮراﻟﯿﻨﺎﺳﻪ‬ ‫ﻗﺮﻣﺰ‬‫ﻣﯽ‬ ‫ﺗﺸﮑﯿﻞ‬ ‫را‬ ‫رﺧﺴﺎره‬ ‫رﯾﺰ‬ ‫اﯾﻦ‬ ‫زﻣﯿﻨﻪ‬ ،‫آ‬‫دﻫﻨﺪ‬‫)ﺷﮑﻞ‬2-H(.
:‫ﺗﻔﺴﯿﺮ‬‫ﺷﻤﺎره‬ ‫رﺧﺴﺎره‬ ‫رﯾﺰ‬ ‫ﻫﻤﺎﻧﻨﺪ‬6‫ﻧﻤﯽ‬ ،‫ﺑﺎﻧﺪﺳﺘﻮﻧﯽ‬ ‫ﺳﺎﺧﺘﺎر‬ ‫و‬ ‫ﺑﺮﺟﺎ‬ ‫ﻓﺎﺑﺮﯾﮏ‬ ‫وﺟﻮد‬ ‫ﻋﺪم‬ ‫ﻋﻠﺖ‬ ‫ﺑﻪ‬ ،‫ﺑﻪ‬ ‫را‬ ‫رﺧﺴﺎره‬ ‫رﯾﺰ‬ ‫اﯾﻦ‬ ‫ﺗﻮان‬
.‫داد‬ ‫ﻧﺴﺒﺖ‬ ‫رﯾﻔﯽ‬ ‫رﺧﺴﺎره‬‫ﮐﻮراﻟﯿﻨﺎﺳﻪ‬ ‫ﺟﻠﺒﮏ‬ ‫ﻫﻤﭽﻨﯿﻦ‬ ‫و‬ ‫ﻣﻨﻔﺬ‬ ‫ﺑﺪون‬ ‫و‬ ‫ﻣﻨﻔﺬدار‬ ‫دﯾﻮاره‬ ‫ﺑﺎ‬ ‫ﻓﺮاﻣﯿﻨﯿﻔﺮﻫﺎي‬ ‫ﺣﻀﻮر‬‫ﺣﺎﮐﯽ‬ ،‫آ‬‫ﭼﺮﺧﺶ‬ ‫از‬
‫ﻣﯽ‬ ‫ﻣﺤﯿﻂ‬ ‫در‬ ‫ﻧﻮر‬ ‫وﺟﻮد‬ ‫ﻫﻤﭽﻨﯿﻦ‬ ‫و‬ ‫آب‬‫ﺳﻤﺖ‬ ‫ﺑﻪ‬ (‫دروﻧﯽ‬ ‫رﻣﭗ‬ ‫)در‬ ‫ﻣﺤﺼﻮر‬ ‫ﻧﯿﻤﻪ‬ ‫ﻻﮔﻮن‬ ‫ﯾﮏ‬ ‫در‬ ً‫ﻻ‬‫اﺣﺘﻤﺎ‬ ‫رﺧﺴﺎره‬ ‫رﯾﺰ‬ ‫اﯾﻦ‬ .‫ﺑﺎﺷﺪ‬
‫ﺗﻪ‬ ‫ﺑﯿﻮﮐﻼﺳﺘﯽ‬ ‫ﺳﺪ‬.‫اﺳﺖ‬ ‫ﺷﺪه‬ ‫ﻧﺸﯿﻦ‬

7. ‫رﯾﺰ‬‫رﺧﺴﺎره‬‫ﻫﺎ‬‫و‬‫ﻣﺪل‬‫رﺳﻮﺑﯽ‬‫ﺳﺎزﻧﺪ‬‫آﺳﻤﺎري‬)‫اﻟﯿﮕﻮﺳﻦ‬(‫در‬‫ﺷﻤﺎل‬‫ﻏﺮب‬‫روﺳﺘﺎي‬‫درﯾﺲ‬...
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9-‫روزن‬ ‫ﭘﻠﻮﺋﯿﺪي‬ ‫ﭘﮑﺴﺘﻮن‬‫ﮐ‬ ‫داران‬‫ﻒ‬‫ﻏﯿﺮﻫﯿﺎﻟﯿﻦ‬ ‫و‬ ‫ﻫﯿﺎﻟﯿﻦ‬ ‫زي‬
Benthic foraminifera (perforate and imperforate) peloidal packstone-2L
:‫ﺗﻮﺻﯿﻒ‬،‫اﻟﻔﯿﺪﯾﻮم‬ ،‫ﻣﯿﻠﯿﻮﻟﯿﺪ‬ ،‫آﺳﺘﺮﯾﮋرﯾﻨﺎ‬ ،‫ﻧﺌﻮروﺗﺎﻟﯿﺎ‬ ،‫ﻫﺘﺮوﺳﺘﮋﯾﻨﺎ‬ ،‫ﻟﭙﯿﺪوﺳﯿﮑﻠﯿﻨﯿﺪه‬ ‫ﺷﺎﻣﻞ‬ ‫رﺧﺴﺎره‬ ‫رﯾﺰ‬ ‫اﯾﻦ‬ ‫در‬ ‫اﺳﮑﻠﺘﯽ‬ ‫اﺟﺰاي‬
،‫دﻧﺪرﯾﺘﯿﻨﺎ‬ ،‫ﻣﺌﺎﻧﺪروﭘﺴﯿﻨﺎ‬ ،‫آﺳﺘﺮوﺗﺮﯾﻠﯿﻨﺎ‬‫ﮐﻮراﻟﯿﻨﺎﺳﻪ‬ ‫ﻗﺮﻣﺰ‬ ‫ﺟﻠﺒﮏ‬ ‫و‬ ‫دﯾﺘﺮوﭘﺎ‬ ،‫واﻟﻮوﻟﯿﻨﯿﺪ‬ ،‫ﺑﻮرﻟﯿﺲ‬‫ﻣﯽ‬ ‫آ‬‫ﺑﺎﺷﺪ‬‫)ﺷﮑﻞ‬2-I(‫اﺟﺰاي‬ .
‫ﻣﯽ‬ ‫ﯾﺎﻓﺖ‬ ‫رﺧﺴﺎره‬ ‫رﯾﺰ‬ ‫اﯾﻦ‬ ‫در‬ ‫ﻓﺮاوان‬ ‫ﻣﯿﺰان‬ ‫ﺑﻪ‬ ‫ﮐﻪ‬ ‫اﺳﺖ‬ ‫ﭘﻠﻮﺋﯿﺪ‬ ‫ﺷﺎﻣﻞ‬ ‫ﻏﯿﺮاﺳﮑﻠﺘﯽ‬.‫ﺷﻮد‬
:‫ﺗﻔﺴﯿﺮ‬‫ﻣ‬ ‫ﺑﺪون‬ ‫اﻧﻮاع‬ ‫ﻫﻤﺮاه‬ ‫ﺑﻪ‬ (‫ﻫﺴﺘﻨﺪ‬ ‫درﯾﺎﯾﯽ‬ ‫ﻧﺮﻣﺎل‬ ‫ﺷﻮري‬ ‫ﻣﻌﺮف‬ ‫)ﮐﻪ‬ ‫ﻫﯿﺎﻟﯿﻦ‬ ‫آﻫﮏ‬ ‫ﺑﺎ‬ ‫ﻣﻨﻔﺬدار‬ ‫ﻓﺮاﻣﯿﻨﯿﻔﺮﻫﺎي‬ ‫ﺣﻀﻮر‬‫ﻨ‬‫آﻫﮏ‬ ‫ﺑﺎ‬ ‫ﻔﺬ‬
‫رﺳﻮب‬ ‫ﺑﯿﺎﻧﮕﺮ‬ ‫ﺑﺮاﯾﻨﮑﻪ‬ ‫ﻋﻼوه‬ ‫رﺧﺴﺎره‬ ‫رﯾﺰ‬ ‫اﯾﻦ‬ ‫در‬ ‫زﯾﺎد‬ ‫ﺗﻨﻮع‬ ‫ﺑﺎ‬ ‫ﭘﺮﺳﻼﻧﻮز‬‫ﻧﯿﻤﻪ‬ ‫ﻻﮔﻮن‬ ‫ﻣﺤﯿﻂ‬ ‫ﯾﮏ‬ ‫در‬ ‫ﮔﺬاري‬‫ﭼ‬ ‫ﺑﺎ‬ ‫ﻣﺤﺼﻮر‬‫ﺮﺧﺶ‬
‫ﻣﯽ‬ ‫داﺧﻠﯽ‬ ‫رﻣﭗ‬ ‫در‬ ‫آب‬ ‫ﻣﺘﻮﺳﻂ‬،‫ﻫﻤﮑﺎران‬ ‫و‬ ‫)روﻣﺮو‬ ‫ﺑﺎﺷﺪ‬2002(‫ﺗﻪ‬ ‫زﻣﺎن‬ ‫در‬ ‫ﮐﻪ‬ ‫اﺳﺖ‬ ‫آن‬ ‫ﻧﻤﺎﯾﺎﻧﮕﺮ‬ ،‫ﺳﺪ‬ ،‫رﺧﺴﺎره‬ ‫اﯾﻦ‬ ‫ﻧﺸﺴﺖ‬
.‫اﺳﺖ‬ ‫ﻧﺪاﺷﺘﻪ‬ ‫وﺟﻮد‬ ‫ﻣﺆﺛﺮي‬
10-‫ﮐﻮراﻟﯿﻨﺎﺳﻪ‬ ‫ﭘﮑﺴﺘﻮن‬‫روزن‬ ‫و‬ ‫آ‬‫ﺑﯿﻮﮐﻼﺳﺖ‬ ‫ﻣﻨﻔﺬ‬ ‫ﺑﺪون‬ ‫داران‬‫دار‬
Bioclastic imperforate foraminifera corallinacean packstone-3L
‫ﮐﻮراﻟﯿﻨﺎﺳﻪ‬ ‫ﻗﺮﻣﺰ‬ ‫ﺟﻠﺒﮏ‬ :‫ﺗﻮﺻﯿﻒ‬‫اﻟﻔﯿﺪﯾﻮ‬ ،‫واﻟﻮوﻟﯿﻨﯿﺪ‬ ،‫آﺳﺘﺮوﺗﺮﯾﻠﯿﻨﺎ‬ ،‫آرﮐﯿﺎس‬ ،‫ﻣﺌﺎﻧﺪروﭘﺴﯿﻨﺎ‬ ‫و‬ ‫اﺻﻠﯽ‬ ‫اﺳﮑﻠﺘﯽ‬ ‫اﺟﺰاي‬ ‫ﻣﯿﻠﯿﻮﻟﯿﺪ‬ ‫و‬ ‫آ‬،‫م‬
‫ﭘﻨﺮوﭘﻠﯿﺲ‬ ،‫رﺋﻮﺳﻼ‬‫ﺧﺮده‬ ‫و‬ ‫اﮐﯿﻨﻮﺋﯿﺪ‬ ،‫دوﮐﻔﻪ‬ ‫ﻫﺎي‬‫آﻟﻮﮐﻢ‬ ‫ﺑﺮﯾﻮزوﺋﺮ‬ ‫و‬ ‫اي‬‫ﺻﻮرت‬ ‫ﺑﻪ‬ ‫اﺟﺰا‬ ‫اﯾﻦ‬ .‫ﻫﺴﺘﻨﺪ‬ ‫رﺧﺴﺎره‬ ‫رﯾﺰ‬ ‫اﯾﻦ‬ ‫ﻓﺮﻋﯽ‬ ‫ﻫﺎي‬
‫)ﺷﮑﻞ‬ ‫دارﻧﺪ‬ ‫ﺣﻀﻮر‬ ‫ﻣﯿﮑﺮاﯾﺖ‬ ‫زﻣﯿﻨﻪ‬ ‫در‬ ‫ﭘﺸﺘﯿﺒﺎن‬ ‫داﻧﻪ‬2-J.(
‫ﮐﻮراﻟﯿﻨﺎﺳﻪ‬ ‫ﻗﺮﻣﺰ‬ ‫ﺟﻠﺒﮏ‬ ‫ﺷﺪه‬ ‫ﺧﺮد‬ ‫ﻗﻄﻌﺎت‬ :‫ﺗﻔﺴﯿﺮ‬‫ﻣﺘﻮﺳﻂ‬ ‫ﭼﺮﺧﺶ‬ ‫ﺑﺎ‬ ‫ﻣﺤﯿﻂ‬ ‫ﯾﮏ‬ ‫از‬ ‫ﺣﺎﮐﯽ‬ ‫رﯾﺰرﺧﺴﺎره‬ ‫اﯾﻦ‬ ‫در‬ ‫ﭘﮑﺴﺘﻮن‬ ‫ﺑﺎﻓﺖ‬ ‫و‬ ‫آ‬
‫آب‬‫ﻣﯽ‬،‫ﺑﺎﺳﯽ‬ ‫و‬ ‫)ﻧﺒﻠﺴﯿﮏ‬ ‫ﺑﺎﺷﺪ‬2000،‫رﺧﺴﺎره‬ ‫رﯾﺰ‬ ‫اﯾﻦ‬ ‫در‬ ‫ﻣﯿﻠﯿﻮﻟﯿﺪ‬ ‫ﺟﻤﻠﻪ‬ ‫از‬ ‫ﭘﺮﺳﻼﻧﻮز‬ ‫دﯾﻮاره‬ ‫ﺑﺎ‬ ‫ﻓﺮاﻣﯿﻨﯿﻔﺮﻫﺎي‬ ‫ﺣﻀﻮر‬ ‫ﻫﻤﭽﻨﯿﻦ‬ .(
‫رﺳﻮب‬‫ﭘﻠﺖ‬ ‫داﺧﻠﯽ‬ ‫)ﺑﺨﺶ‬ ‫ﻣﺤﺼﻮر‬ ً‫ﺎ‬‫ﻧﺴﺒﺘ‬ ‫ﻣﺤﯿﻂ‬ ‫ﯾﮏ‬ ‫در‬ ‫ﮔﺬاري‬‫ﻣﯽ‬ ‫ﺑﯿﺎن‬ ‫را‬ (‫ﮐﺮﺑﻨﺎﺗﻪ‬ ‫ﻓﺮم‬.‫ﮐﻨﺪ‬
11-‫ﭘﮑﺴﺘﻮن‬-‫ﺑﯿﻮﮐﻼﺳﺖ‬ ‫ﮔﺮﯾﻨﺴﺘﻮن‬‫روزن‬ ‫ﺑﺎ‬ ‫ﻫﻤﺮاه‬ ‫دار‬‫ﻣ‬ ‫ﻣﻨﻔﺬ‬ ‫ﺑﺪون‬ ‫داران‬‫ﺘﻨﻮع‬
grainstone-High diversity imperforate foraminifera bioclastic packstone-4L
‫روزن‬ :‫ﺗﻮﺻﯿﻒ‬‫ﮐﻒ‬ ‫داران‬،‫ﻣﺌﺎﻧﺪروﭘﺴﯿﻨﺎ‬ ،‫ﻣﯿﻠﯿﻮﻟﯿﺪ‬ ،‫اﺳﭙﯿﺮوﻟﯿﻨﺎ‬ ،‫آﺳﺘﺮوﺗﺮﯾﻠﯿﻨﺎ‬ ،‫آرﮐﯿﺎس‬ ،‫ﭘﻨﺮوﭘﻠﯿﺲ‬ ‫ﻗﺒﯿﻞ‬ ‫از‬ ‫ﻣﻨﻔﺬ‬ ‫ﺑﺪون‬ ‫دﯾﻮاره‬ ‫ﺑﺎ‬ ‫زي‬
‫اﺳﭙﯿﺮوﻟﻮﮐﻮ‬ ،‫ﺗﮑﺴﺘﻮﻻرﯾﺪ‬ ،‫ﭘﯿﺮﮔﻮ‬ ،‫دﻧﺪرﯾﺘﯿﻨﺎ‬ ،‫واﻟﻮوﻟﯿﻨﯿﺪ‬‫ﺟﻠ‬ ،‫اﺳﺘﺮاﮐﻮد‬ ،‫ﺑﺮﯾﻮزوﺋﺮ‬ ،‫اﻟﻔﯿﺪﯾﻮم‬ ،‫دﯾﺴﮑﻮرﺑﯿﺲ‬ ‫ﻫﻤﺮاه‬ ‫ﺑﻪ‬ ‫ﻟﯿﻨﺎ‬‫ﻗﺮﻣﺰ‬ ‫ﺒﮏ‬
‫ﮐﻮراﻟﯿﻨﺎﺳﻪ‬‫داﺳﯽ‬ ‫ﺳﺒﺰ‬ ‫ﺟﻠﺒﮏ‬ ،‫آ‬‫ﮐﻼداﺳﻪ‬‫دوﮐﻔﻪ‬ ،‫آ‬‫ﺑﻪ‬ ‫رﺧﺴﺎره‬ ‫رﯾﺰ‬ ‫اﯾﻦ‬ ‫ﺑﺎﻓﺖ‬ .‫دارﻧﺪ‬ ‫ﺣﻀﻮر‬ ‫رﺧﺴﺎره‬ ‫رﯾﺰ‬ ‫اﯾﻦ‬ ‫در‬ ‫ﮔﺎﺳﺘﺮوﭘﻮد‬ ‫و‬ ‫اي‬
‫آﻟﻮﮐﻢ‬ ‫اﻧﺪازه‬ .‫اﺳﺖ‬ ‫ﮔﺮﯾﻨﺴﺘﻮن‬ ‫ﺗﺎ‬ ‫ﭘﮑﺴﺘﻮن‬ ‫ﺻﻮرت‬‫ﺑﻪ‬ ‫ﻫﺎ‬‫ﺟﻮرﺷﺪﮔ‬ ‫و‬ ‫ﺑﻮده‬ ‫درﺷﺖ‬ ‫ﺗﺎ‬ ‫رﯾﺰ‬ ‫ﺻﻮرت‬‫دارﻧ‬ ‫ﻣﺘﻮﺳﻂ‬ ‫ﺗﺎ‬ ‫ﺿﻌﯿﻒ‬ ‫ﯽ‬‫)ﺷﮑﻞ‬ ‫ﺪ‬
2-K‫ﻓﺮاوان‬ ‫رﺧﺴﺎره‬ ‫رﯾﺰ‬ ‫اﯾﻦ‬ ‫ﺿﺨﺎﻣﺖ‬ ‫ﻧﻈﺮ‬ ‫از‬ .(‫ﺿﺨﺎﻣﺖ‬ ‫از‬ ‫و‬ ‫اﺳﺖ‬ ‫درﯾﺲ‬ ‫ﺑﺮش‬ ‫در‬ ‫رﺧﺴﺎره‬ ‫ﺗﺮﯾﻦ‬267‫ﺑﺮش‬ ‫اﻧﺘﻬﺎي‬ ‫ﺗﺎ‬ ‫ﻣﺘﺮ‬
‫رﺧﺴﺎره‬ ‫ﺑﻪ‬ ‫ﻣﺘﻨﺎوب‬ ‫ﺻﻮرت‬ ‫ﺑﻪ‬ ‫ﻣﻄﺎﻟﻌﻪ‬ ‫ﻣﻮرد‬‫)رﺧﺴﺎره‬ ‫ﻣﺠﺎور‬ ‫ﻫﺎي‬‫ﻣﯽ‬ ‫ﺗﻐﯿﯿﺮ‬ (‫دروﻧﯽ‬ ‫رﻣﭗ‬ ‫در‬ ‫ﻓﻠﺖ‬ ‫ﺗﺎﯾﺪال‬ ‫و‬ ‫ﻻﮔﻮن‬ ‫ﻫﺎي‬.‫ﯾﺎﺑﺪ‬
‫داﻧﻪ‬ ‫ﻓﺎﺑﺮﯾﮏ‬ :‫ﺗﻔﺴﯿﺮ‬‫رﺳﻮب‬ ‫از‬ ‫ﺣﺎﮐﯽ‬ ،‫ﺑﺎﻻ‬ ‫ﺗﻨﻮع‬ ‫ﺑﺎ‬ ‫ﻣﻨﻔﺬ‬ ‫ﺑﺪون‬ ‫دﯾﻮاره‬ ‫ﺑﺎ‬ ‫ﻓﺮاﻣﯿﻨﯿﻔﺮﻫﺎي‬ ‫ﺣﻀﻮر‬ ‫و‬ ‫ﭘﺸﺘﯿﺒﺎن‬‫ﮔﺬاري‬‫ﻻﮔﻮن‬ ‫ﯾﮏ‬ ‫در‬
‫ﮐﻢ‬‫ﻣﯽ‬ ‫داﺧﻠﯽ‬ ‫رﻣﭗ‬ ‫در‬ ‫ﭘﺮﻧﻮر‬ ‫و‬ ‫ﻣﺤﺼﻮر‬ ً‫ﺎ‬‫ﻧﺴﺒﺘ‬ ‫ﻋﻤﻖ‬،‫)ﮔﯿﻞ‬ ‫ﺑﺎﺷﺪ‬2000‫رﺧﺴﺎره‬ .(‫ﺳﺎزﻧﺪ‬ ‫داﺧﻠﯽ‬ ‫رﻣﭗ‬ ‫ﺑﺨﺶ‬ ‫از‬ ‫ﻧﯿﺰ‬ ‫ﻣﺸﺎﺑﻪ‬ ‫ﻫﺎي‬
‫)وزﯾﺮي‬ ‫اﺳﺖ‬ ‫ﺷﺪه‬ ‫ﻣﻌﺮﻓﯽ‬ ‫زاﮔﺮس‬ ‫رﺳﻮﺑﯽ‬ ‫ﺣﻮﺿﻪ‬ ‫در‬ ‫آﺳﻤﺎري‬‫ﻫﻤ‬ ‫و‬ ‫ﻣﻘﺪم‬،‫ﮑﺎران‬2010،‫ﻫﻤﮑﺎران‬ ‫و‬ ‫ﺻﺎدﻗﯽ‬ ‫؛‬2010‫ﺳﻠﻄﺎﻧﯿﺎن‬ ‫؛‬
،‫ﻫﻤﮑﺎران‬ ‫و‬2011.(

8. ‫رﯾﺰ‬‫رﺧﺴﺎره‬‫ﻫﺎ‬‫و‬‫ﻣﺪل‬‫رﺳﻮﺑﯽ‬‫ﺳﺎزﻧﺪ‬‫آﺳﻤﺎري‬)‫اﻟﯿﮕﻮﺳﻦ‬(‫در‬‫ﺷﻤﺎل‬‫ﻏﺮب‬‫روﺳﺘﺎي‬‫درﯾﺲ‬...
٨
12-‫وﮐﺴﺘﻮن‬-‫ﺑﯿﻮﮐﻼﺳﺖ‬ ‫ﻣﯿﻠﯿﻮﻟﯿﺪ‬ ‫ﭘﮑﺴﺘﻮن‬‫دار‬
packstone-Bioclastic miliolids wackestone-5L
‫ﻓﺮاوان‬ ‫ﻋﻨﻮان‬ ‫ﺑﻪ‬ ‫ﻣﯿﻠﯿﻮﻟﯿﺪ‬ :‫ﺗﻮﺻﯿﻒ‬‫ﻣﯽ‬ ‫رﺧﺴﺎره‬ ‫رﯾﺰ‬ ‫اﯾﻦ‬ ‫در‬ ‫اﺳﮑﻠﺘﯽ‬ ‫داﻧﻪ‬ ‫ﺗﺮﯾﻦ‬‫ﺑ‬ ‫دﻟﯿﻞ‬ ‫ﺑﻪ‬ ‫ﻣﻘﺎﻃﻊ‬ ‫از‬ ‫ﺑﺮﺧﯽ‬ ‫در‬ .‫ﺑﺎﺷﺪ‬‫ﯿ‬‫ﺶ‬‫ﺷﺪن‬ ‫ﺗﺮ‬
‫وﮐﺴﺘﻮن‬ ‫رﺧﺴﺎره‬ ‫رﯾﺰ‬ ‫زﯾﺮ‬ ‫واﻟﻮوﻟﯿﻨﯿﺪ‬-‫ﺑﯿﻮﮐﻼﺳﺖ‬ ‫ﻣﯿﻠﯿﻮﻟﯿﺪ‬ ‫و‬ ‫واﻟﻮوﻟﯿﻨﯿﺪ‬ ‫ﭘﮑﺴﺘﻮن‬‫ﻣﯽ‬ ‫ﻣﻌﺮﻓﯽ‬ ‫دار‬‫)ﺷﮑﻞ‬ ‫ﺷﻮد‬2-L:(
packstone-Bioclastic miliolids Valvulinid wackestone-1-5L
‫آﻟﻮﮐﻢ‬ ‫ﺳﺎﯾﺮ‬‫ﺧﺮده‬ ‫و‬ ‫دﻧﺪرﯾﺘﯿﻨﺎ‬ ،‫آﺳﺘﺮوﺗﺮﯾﻠﯿﻨﺎ‬ ،‫آرﮐﯿﺎس‬ ،‫اﻟﻔﯿﺪﯾﻮم‬ ‫ﻫﺎ‬‫دوﮐﻔﻪ‬ ‫ﻫﺎي‬‫ﻣﯽ‬ ‫اي‬.‫ﺑﺎﺷﺪ‬
‫ﮔﻞ‬ ‫ﻓﺎﺑﺮﯾﮏ‬ :‫ﺗﻔﺴﯿﺮ‬‫ﻣﯿﻠﯿﻮﻟﯿﺪ‬ ‫ﻫﻤﺮاه‬ ‫ﺑﻪ‬ ‫ﭘﺸﺘﯿﺒﺎن‬‫ﺗﺎﮐﺴﻮن‬ ‫ﮐﻢ‬ ‫ﺗﻨﻮع‬ ‫و‬ (‫ﻧﻮر‬ ‫زﯾﺎد‬ ‫ﺷﺪت‬ ‫ﻋﻠﺖ‬ ‫)ﺑﻪ‬ ‫ﺿﺨﯿﻢ‬ ‫دﯾﻮاره‬ ‫ﺑﺎ‬ ‫ﻫﺎي‬‫ﻫ‬‫از‬ ‫ﺣﺎﮐﯽ‬ ‫ﺎ‬
‫ﮐﻢ‬ ‫ﻻﮔﻮن‬ ‫ﯾﮏ‬ ‫در‬ ‫رﺧﺴﺎره‬ ‫رﯾﺰ‬ ‫اﯾﻦ‬ ‫ﺗﺸﮑﯿﻞ‬‫ﻣﯽ‬ ‫اﻧﺪك‬ ‫ﻫﯿﺪروﻟﯿﮑﯽ‬ ‫ﭼﺮﺧﺶ‬ ‫ﺑﺎ‬ ‫ﻋﻤﻖ‬،‫)ﮔﯿﻞ‬ ‫ﺑﺎﺷﺪ‬2000،‫ﻓﻠﻮﮔﻞ‬ ‫؛‬2010‫ﻣﺸﺎﺑﻪ‬ .(
‫زاﮔﺮس‬ ‫رﺳﻮﺑﯽ‬ ‫ﺣﻮﺿﻪ‬ ‫در‬ ‫رﺧﺴﺎره‬ ‫رﯾﺰ‬ ‫اﯾﻦ‬‫)اﷲ‬ ‫اﺳﺖ‬ ‫ﺷﺪه‬ ‫ﮔﺰارش‬ ‫ﻧﯿﺰ‬ ‫ﮔﭽﺴﺎران‬ ‫ﺷﻤﺎل‬ ‫در‬‫ﮐﺮم‬،‫ﻫﻤﮑﺎران‬ ‫و‬ ‫دﯾﻞ‬ ‫ﭘﻮر‬2010(
13-‫ﺑﯿﻮﮐﻼﺳﺖ‬ ‫وﮐﺴﺘﻮن‬‫ﮐﻮﭼﮏ‬ ‫روﺗﺎﻟﯿﺎﻫﺎي‬ ‫و‬ ‫دﯾﺴﮑﻮرﺑﯿﺲ‬ ‫ﺣﺎوي‬ ‫دار‬
Discorbis small rotaliids bioclastic wackestone-6L
‫ﻣﯽ‬ ‫ﻣﺸﺨﺺ‬ ‫دﯾﺴﮑﻮرﺑﯿﺲ‬ ‫ﺟﻨﺲ‬ ‫و‬ ‫ﮐﻮﭼﮏ‬ ‫روﺗﺎﻟﯿﺎﻫﺎي‬ ‫ﻓﺮاواﻧﯽ‬ ‫ﺑﺎ‬ ‫رﺧﺴﺎره‬ ‫رﯾﺰ‬ ‫اﯾﻦ‬ :‫ﺗﻮﺻﯿﻒ‬‫ﺷﻮد‬‫)ﺷﮑﻞ‬2-M‫ﻫﻤﭽﻨﯿﻦ‬ .(
‫ﮐﻮراﻟﯿﻨﺎﺳﻪ‬ ‫ﻗﺮﻣﺰ‬ ‫ﺟﻠﺒﮏ‬ ‫و‬ ‫واﻟﻮوﻟﯿﻨﯿﺪ‬ ،‫اﻟﻔﯿﺪﯾﻮم‬ ،‫ﻣﯿﻠﯿﻮﻟﯿﺪ‬ ،‫رﺋﻮﺳﻼ‬‫ﮐﻢ‬ ‫ﻣﯿﺰان‬ ‫ﺑﻪ‬ ‫آ‬‫آﻟﻮﮐﻢ‬ .‫دارﻧﺪ‬ ‫وﺟﻮد‬ ‫ﺗﺮ‬‫ﮔ‬ ‫ﺻﻮرت‬ ‫ﺑﻪ‬ ‫ﻫﺎ‬‫ﻞ‬‫ﭘﺸﺘﯿﺒﺎن‬
‫ﺧﺮده‬ ‫و‬ ‫ﻣﯿﮑﺮاﯾﺖ‬ ‫زﻣﯿﻨﻪ‬ ‫ﯾﮏ‬ ‫در‬.‫دارﻧﺪ‬ ‫ﺣﻀﻮر‬ ،‫ﺑﯿﻮﮐﻼﺳﺖ‬ ‫ﻫﺎي‬
‫ﺑﯿﺎن‬ ‫رﺧﺴﺎره‬ ‫رﯾﺰ‬ ‫اﯾﻦ‬ ‫ﺑﻮدن‬ ‫ﭘﺸﺘﯿﺒﺎن‬ ‫ﮔﻞ‬ :‫ﺗﻔﺴﯿﺮ‬‫رﺳﻮب‬ ‫ﮐﻨﻨﺪه‬‫ﯾﮏ‬ ‫در‬ ‫ﮔﺬاري‬‫ﻣﯽ‬ ‫ﺑﺴﺘﻪ‬ ‫ﻣﺤﯿﻂ‬ ‫ﯾﮏ‬ ‫در‬ ‫ﮐﻢ‬ ‫اﻧﺮژي‬ ‫ﺑﺎ‬ ‫ﺷﺮاﯾﻂ‬.‫ﺑﺎﺷﺪ‬
‫ﺗﺎﮐﺴﻮن‬ ‫ﻓﺮاواﻧﯽ‬ ‫و‬ ‫ﺗﻨﻮع‬ ‫ﻋﺪم‬ ‫ﻫﻤﭽﻨﯿﻦ‬‫ﮔﺮدش‬ ‫ﺑﺎ‬ ‫ﻣﺤﺪود‬ ‫ﻣﺤﯿﻂ‬ ‫ﺷﺮاﯾﻂ‬ ،‫ﺣﺮارت‬ ‫درﺟﻪ‬ ً‫ﻻ‬‫اﺣﺘﻤﺎ‬ ‫و‬ ‫آب‬ ‫ﺷﻮري‬ ‫رﻓﺘﻦ‬ ‫ﺑﺎﻻ‬ ‫اﺛﺮ‬ ‫در‬ ‫ﻫﺎ‬
‫ﻣﯽ‬ ‫ﺗﺄﯾﯿﺪ‬ ‫را‬ ‫اﻧﺪك‬ ‫آب‬‫ﻣﯽ‬ ‫ﻣﺤﺪود‬ ‫و‬ ‫ﺑﺴﺘﻪ‬ ‫رﺳﻮﺑﯽ‬ ‫ﻣﺤﯿﻂ‬ ‫ﯾﮏ‬ ‫در‬ ‫رﺧﺴﺎره‬ ‫رﯾﺰ‬ ‫اﯾﻦ‬ .‫ﮐﻨﺪ‬‫ﺟﺰ‬ ‫ﭘﻬﻨﻪ‬ ‫روﺑﻪ‬ ‫ﻻﮔﻮن‬ ‫ﺑﺨﺶ‬ ‫در‬ ‫ﺗﻮاﻧﺪ‬‫ر‬‫وﻣﺪي‬
‫ﻓﻮق‬ ‫ﯾﺎ‬ ‫ﺷﻮر‬ ‫آب‬ ‫ﮐﻪ‬،‫)وﯾﻠﺴﻮن‬ ‫ﺑﺎﺷﺪ‬ ‫ﺷﺪه‬ ‫ﺗﺸﮑﯿﻞ‬ ‫اﺳﺖ‬ ‫ﺷﻮر‬ ‫اﻟﻌﺎده‬1975،‫ﻫﻤﮑﺎران‬ ‫و‬ ‫داﻧﯿﻞ‬ ‫؛‬2008،‫ﻓﻠﻮﮔﻞ‬ ‫؛‬2010.(
14-‫ﮐﻮارﺗﺰدار‬ ‫ﻣﺎدﺳﺘﻮن‬
T- Sandy mudstone
:‫ﺗﻮﺻﯿﻒ‬‫داﻧﻪ‬ ‫داراي‬ ‫و‬ ‫ﺑﻮده‬ ‫اﺳﮑﻠﺘﯽ‬ ‫آﺛﺎر‬ ‫ﻓﺎﻗﺪ‬ ‫رﺧﺴﺎره‬ ‫رﯾﺰ‬ ‫اﯾﻦ‬‫ﺗﺨﺮﯾﺒﯽ‬ ‫ﻫﺎي‬‫ﻣﯽ‬ ‫ﻣﯿﮑﺮاﯾﺖ‬ ‫زﻣﯿﻨﻪ‬ ‫ﯾﮏ‬ ‫در‬ ‫ﮐﻮارﺗﺰ‬‫ﺑﺎﺷ‬‫اﺛﺮ‬ ‫در‬ ‫ﮐﻪ‬ ‫ﺪ‬
‫ﺗﺎﯾﺪال‬ ‫ﺑﺨﺶ‬ ‫در‬ ‫ﺗﺨﺮﯾﺒﯽ‬ ‫ﻣﻮاد‬ ‫ورود‬‫اﺳﺖ‬ ‫ﺷﺪه‬ ‫ﺗﺸﮑﯿﻞ‬ ‫ﻓﻠﺖ‬‫)ﺷﮑﻞ‬2-N(.‫ﺑﺎﻻي‬ ‫ﺷﻮري‬ ‫دﻟﯿﻞ‬ ‫ﺑﻪ‬ ‫اﺣﺘﻤﺎﻻ‬ ‫زﯾﺴﺘﯽ‬ ‫آﺛﺎر‬ ‫وﺟﻮد‬ ‫ﻋﺪم‬
‫ﻣﯽ‬ ‫ﻣﺤﯿﻂ‬ ‫اﯾﻦ‬ ‫در‬ ‫آب‬‫)اﷲ‬ ‫اﺳﺖ‬ ‫ﺷﺪه‬ ‫ﻣﺸﺎﻫﺪه‬ ‫ﻧﯿﺰ‬ ‫ﮔﭽﺴﺎران‬ ‫ﺷﻤﺎل‬ ‫در‬ ‫رﺧﺴﺎره‬ ‫رﯾﺰ‬ ‫اﯾﻦ‬ ‫ﻣﺸﺎﺑﻪ‬ .‫ﺑﺎﺷﺪ‬‫ﻫﻤﮑﺎران‬ ‫و‬ ‫ﭘﻮر‬ ‫ﮐﺮم‬،2010.(
‫ﺿﺨﺎﻣﺖ‬ ‫از‬ ‫ﻣﻄﺎﻟﻌﻪ‬ ‫ﺑﺮش‬159‫ﺗﺎ‬221‫ﺗﻮده‬ ‫دوﻟﻮﻣﯿﺖ‬ ‫ﺷﺎﻣﻞ‬ ‫ﻣﺘﺮ‬‫)ﺷﮑﻞ‬ ‫اﺳﺖ‬ ‫ﻻﯾﻪ‬ ‫ﻣﺘﻮﺳﻂ‬ ‫ﺗﺎ‬ ‫ﺿﺨﯿﻢ‬ ‫و‬ ‫اي‬3‫دوﻟﻮﻣﯿﺖ‬ ‫اﯾﻦ‬ ‫رﻧﮓ‬ .(‫ﻫﺎ‬
‫ﻣﯽ‬ ‫ﺳﻔﯿﺪ‬ ‫ﻧﺎزك‬ ‫ﻣﻘﺎﻃﻊ‬ ‫در‬‫دوﻟﻮﻣﯿﺖ‬ .‫ﺑﺎﺷﺪ‬‫دوﻟﻮﻣﯿﺖ‬ ‫ﻧﻮع‬ ‫از‬ ‫و‬ ‫داﺷﺘﻪ‬ ‫ﺟﺎﻧﺸﯿﻨﯽ‬ ‫ﻣﻨﺸﺄ‬ ‫ﻣﻮﺟﻮد‬ ‫ﻫﺎي‬‫دوم‬ ‫ﻧﻮع‬ ‫ﻫﺎي‬
‫ﻣﯽ‬ (‫)دوﻟﻮﻣﯿﮑﺮواﺳﭙﺎراﯾﺖ‬‫ﺻﻮرﺗﯽ‬ ‫ﺑﻪ‬ ‫ﺑﺎﺷﻨﺪ‬‫ﺑﺎﻓ‬ ‫ﮐﻪ‬‫ﺖ‬‫ﺑﻪ‬ ‫ﻓﺴﯿﻠﯽ‬ ‫آﺛﺎر‬ ‫و‬ ‫اوﻟﯿﻪ‬ ‫رﺳﻮﺑﯽ‬ ‫ﻫﺎي‬‫رﻓﺘﻪ‬ ‫ﺑﯿﻦ‬ ‫از‬ ‫ﮐﺎﻣﻞ‬ ‫ﻃﻮر‬‫ا‬‫و‬ ‫)آداﺑﯽ‬ ‫ﻧﺪ‬
،‫ﻫﻤﮑﺎران‬1996‫رﺧﺴﺎره‬ ‫رﯾﺰ‬ ،‫ﻣﻄﺎﻟﻌﻪ‬ ‫ﺑﺮش‬ ‫از‬ ‫ﺿﺨﺎﻣﺖ‬ ‫اﯾﻦ‬ ‫ﺑﺮاي‬ ‫ﺑﻨﺎﺑﺮاﯾﻦ‬ .(‫ﻧﻤﯽ‬ ‫ﻣﻌﺮﻓﯽ‬ ‫اي‬،‫دوﻟﻮﻣﯿﺖ‬ ‫ﺑﻠﻮرﻫﺎي‬ ‫اﻧﺪازه‬ .‫ﺷﻮد‬
‫ﺷﮑﻞ‬ ‫ﺻﻮرت‬ ‫ﺑﻪ‬ ‫اﻏﻠﺐ‬ ‫و‬ ‫ﺑﻮده‬ ‫ﻣﺘﻮﺳﻂ‬ ‫ﺗﺎ‬ ‫درﺷﺖ‬‫ﻣﯽ‬ ‫را‬ ‫ﺳﻨﮓ‬ ‫ﭼﻬﺎرﭼﻮب‬ ‫و‬ ‫ﻫﺴﺘﻨﺪ‬ ‫دار‬‫ﺳﺎزﻧﺪ‬‫)ﺷﮑﻞ‬2-O(.

9. ‫رﯾﺰ‬‫رﺧﺴﺎره‬‫ﻫﺎ‬‫و‬‫ﻣﺪل‬‫رﺳﻮﺑﯽ‬‫ﺳﺎزﻧﺪ‬‫آﺳﻤﺎري‬)‫اﻟﯿﮕﻮﺳﻦ‬(‫در‬‫ﺷﻤﺎل‬‫ﻏﺮب‬‫روﺳﺘﺎي‬‫درﯾﺲ‬...
٩
‫ﺷﮑﻞ‬2-‫رﺧﺴﺎره‬ ‫رﯾﺰ‬.‫درﯾﺲ‬ ‫ﺑﺮش‬ ‫در‬ ‫آﺳﻤﺎري‬ ‫ﺳﺎزﻧﺪ‬ ‫ﻫﺎي‬
A: O1- Bioclastic nummulitidae floatstone-rudstone, sample no. B5; B: O2- Bioclastic nummulitidae
lepidocyclinidae Neorotalia rudstone, sample no.B56; C: O3- Bioclastic Neorotalia nummulitidae packstone-
rudstone, sample no. B17; D: O4- Bioclastic Neorotalia lepidocyclinidae packstone, sample no. B85; E: O5-
Bioclastic Neorotalia corallinacean packstone, sample no. B69; F: O6- Bioclastic coral corallinacean Neorotalia
packstone-rudstone, sample no. B135; G: Sh- Neorotalia corallinacean echinoids packstone-grainstone, sample
no. B100; H: L1- Coral benthic foraminifera floatstone-rudstone, sample no. B435; I: L2- Benthic foraminifera
(perforate and imperforate) peloidal packstone, sample no. B225; J: L3- Bioclastic imperforate foraminifera
corallinacean packstone, sample no. B437; K: L4- High diversity imperforate foraminifera bioclastic packstone-
grainstone, sample no. B454; L: L5-1- Bioclastic miliolids Valvulinid wackestone-packstone, sample no. B365;
M: L6- Discorbis small rotaliids bioclastic wackestone, sample no. B252; N: T- Sandy mudstone, sample no.
B396; O: Dolomite in xpl light, sample no. B175.
Archaias (A), Austrotrillina (As), bioclast fragment (Bio), Bryozoan (Br), coral fragment (C), Discorbis (D),
echinoids (E), Elphidium (El), Heterostegina (H), lepidocyclinids (Lep), miliolids (M), Meandropsina (Me),

10. ‫رﯾﺰ‬‫رﺧﺴﺎره‬‫ﻫﺎ‬‫و‬‫ﻣﺪل‬‫رﺳﻮﺑﯽ‬‫ﺳﺎزﻧﺪ‬‫آﺳﻤﺎري‬)‫اﻟﯿﮕﻮﺳﻦ‬(‫در‬‫ﺷﻤﺎل‬‫ﻏﺮب‬‫روﺳﺘﺎي‬‫درﯾﺲ‬...
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Nummulites (N), Operculina (Op), Peneroplis (P), peloid (Pel), Neorotalia (R), corallinacean (Ral), Reussella
(Re), textularids (T), Valvulinid (V).
‫ﺷﮑﻞ‬3-‫رﺧﺴﺎره‬ ‫رﯾﺰ‬ ‫ﺳﺘﻮن‬.(‫ﻓﺎرس‬ ‫اﺳﺘﺎن‬ ‫)ﻏﺮب‬ ‫درﯾﺲ‬ ‫ﺑﺮش‬ ‫در‬ ‫آﺳﻤﺎري‬ ‫ﺳﺎزﻧﺪ‬ ‫آب‬ ‫ﺳﻄﺢ‬ ‫ﺗﻐﯿﯿﺮات‬ ‫و‬ ‫رﺳﻮﺑﯽ‬ ‫ﻣﺤﯿﻂ‬ ،‫ﻫﺎ‬
4-2-‫رﺳﻮﺑﯽ‬ ‫ﻣﺤﯿﻂ‬
‫ﺗﺎﮐﺴﻮن‬ ‫ﻣﻄﺎﻟﻌﻪ‬ ‫اﺳﺎس‬ ‫ﺑﺮ‬‫رﺧﺴﺎره‬ ‫رﯾﺰ‬ ‫ﻋﻤﻮدي‬ ‫ﺗﻐﯿﯿﺮات‬ ‫و‬ ‫ﻣﯿﮑﺮوﺳﮑﻮﭘﯽ‬ ‫ﻣﻘﺎﻃﻊ‬ ‫رﺳﻮﺑﯽ‬ ‫ﺑﺎﻓﺖ‬ ،‫ﻫﺎ‬‫آﺳ‬ ‫ﺳﺎزﻧﺪ‬ ‫رﺳﻮﺑﯽ‬ ‫ﻣﺪل‬ ،‫ﻫﺎ‬‫ﻤﺎري‬
‫ﻣﻄﺎﻟﻌﻪ‬ ‫ﺑﺮش‬ ‫در‬‫رﺧﺴﺎره‬ ‫ﺗﺪرﯾﺠﯽ‬ ‫ﺗﻐﯿﯿﺮات‬ ‫و‬ ‫ﺑﯿﻮﮐﻼﺳﺘﯽ‬ ‫ﺳﺪ‬ ‫وﺟﻮد‬ ‫دﻟﯿﻞ‬ ‫ﺑﻪ‬ .‫اﺳﺖ‬ ‫ﮔﺮدﯾﺪه‬ ‫ﻣﻌﺮﻓﯽ‬‫ﻣﻮار‬ ‫وﺟﻮد‬ ‫ﻋﺪم‬ ‫ﻧﯿﺰ‬ ‫و‬ ‫ﻫﺎ‬‫دي‬
‫ﺟﺮﯾﺎن‬ ‫از‬ ‫ﻧﺎﺷﯽ‬ ‫رﺳﻮﺑﺎت‬ ‫و‬ ‫ﺗﻮرﺑﯿﺪاﯾﺖ‬ ،‫رﯾﺰش‬ ‫آﺛﺎر‬ ‫ﻫﻤﭽﻮن‬‫ﭘﻠﺖ‬ ،‫ﺑﺮﺟﺎ‬ ‫ﮔﺴﺘﺮده‬ ‫رﯾﻒ‬ ‫وﺟﻮد‬ ‫ﻋﺪم‬ ‫ﻫﻤﭽﻨﯿﻦ‬ ‫و‬ ‫آﺷﻔﺘﻪ‬ ‫ﻫﺎي‬‫ﻓ‬‫ﺮم‬
‫ﭘﯿﺸﻨﻬﺎد‬ ‫درﯾﺲ‬ ‫ﺑﺮش‬ ‫در‬ ‫آﺳﻤﺎري‬ ‫ﺳﺎزﻧﺪ‬ ‫ﺑﺮاي‬ ‫ﻫﻤﻮﮐﻠﯿﻨﺎل‬ ‫رﻣﭗ‬ ‫ﮐﺮﺑﻨﺎﺗﻪ‬‫ﻣﯽ‬،‫)ﮔﯿﻞ‬ ‫ﺷﻮد‬2000‫دو‬ ‫ﺷﺎﻣﻞ‬ ‫ﻫﻤﻮﮐﻠﯿﻨﺎل‬ ‫رﻣﭗ‬ ‫اﯾﻦ‬ .(

11. ‫رﯾﺰ‬‫رﺧﺴﺎره‬‫ﻫﺎ‬‫و‬‫ﻣﺪل‬‫رﺳﻮﺑﯽ‬‫ﺳﺎزﻧﺪ‬‫آﺳﻤﺎري‬)‫اﻟﯿﮕﻮﺳﻦ‬(‫در‬‫ﺷﻤﺎل‬‫ﻏﺮب‬‫روﺳﺘﺎي‬‫درﯾﺲ‬...
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‫رﺧﺴﺎره‬ ‫وﺟﻮد‬ ‫ﻋﺪم‬ ‫دﻟﯿﻞ‬ ‫ﺑﻪ‬ .‫اﺳﺖ‬ ‫ﻣﯿﺎﻧﯽ‬ ‫رﻣﭗ‬ ‫و‬ ‫دروﻧﯽ‬ ‫رﻣﭗ‬ ‫ﺑﺨﺶ‬‫رﻣﭗ‬ ،‫ﭘﻼﻧﮑﺘﻮن‬ ‫ﻓﺮاﻣﯿﻨﯿﻔﺮﻫﺎي‬ ‫و‬ ‫درﯾﺎﯾﯽ‬ ‫ﻋﻤﯿﻖ‬ ‫ﻣﺤﯿﻂ‬ ‫ﻫﺎي‬
‫ﻧﻤﯽ‬ ‫ﭘﯿﺸﻨﻬﺎد‬ ‫رﺳﻮﺑﯽ‬ ‫ﻣﺤﯿﻂ‬ ‫اﯾﻦ‬ ‫ﺑﺮاي‬ ‫ﺑﯿﺮوﻧﯽ‬‫)ﺷﮑﻞ‬ ‫ﮔﺮدد‬4.(‫ﮐﻢ‬ ‫و‬ ‫ﻋﻤﯿﻖ‬ ‫ﺑﺨﺶ‬ ‫دو‬ ‫ﺑﻪ‬ ‫ﻣﯿﺎﻧﯽ‬ ‫رﻣﭗ‬ ‫ﻣﺤﯿﻂ‬‫ﻣﯽ‬ ‫ﺗﻘﺴﯿﻢ‬ ‫ﻋﻤﻖ‬.‫ﺷﻮد‬
‫رﺧﺴﺎره‬ ‫رﯾﺰ‬ ‫ﺷﺎﻣﻞ‬ ‫ﻣﯿﺎﻧﯽ‬ ‫رﻣﭗ‬ ‫ﻋﻤﯿﻖ‬ ‫ﻗﺴﻤﺖ‬‫ﻫﺎي‬1O،2O‫و‬3O‫ﯾﮏ‬ ‫در‬ ‫ﮐﺸﯿﺪه‬ ‫دﯾﻮاره‬ ‫ﺑﺎ‬ ‫ﻫﯿﺎﻟﯿﻦ‬ ‫ﻓﺮاﻣﯿﻨﯿﻔﺮﻫﺎي‬ ‫داراي‬ ‫ﮐﻪ‬ ‫اﺳﺖ‬
‫ﻣﯽ‬ ‫رودﺳﺘﻮن‬ ‫ﺗﺎ‬ ‫ﻓﻠﻮﺗﺴﺘﻮن‬ ‫ﺑﺎﻓﺖ‬‫ﮔﺸﺘﻪ‬ ‫ﺗﺸﮑﯿﻞ‬ ‫روﭘﻠﯿﻦ‬ ‫زﻣﺎن‬ ‫در‬ ‫و‬ ‫ﺑﺎﺷﻨﺪ‬‫ﮐﻢ‬ ‫ﻗﺴﻤﺖ‬ .‫اﻧﺪ‬‫ﻋﻤﻖ‬‫ﺿﺨ‬ ‫ﺑﺎ‬ ‫ﻣﯿﺎﻧﯽ‬ ‫رﻣﭗ‬ ‫ﺗﺮ‬‫ﻋﺪﺳﯽ‬ ‫و‬ ‫ﯿﻢ‬‫ﺗﺮ‬
‫ﻟﭙ‬ ‫و‬ ‫ﻧﻮﻣﻮﻟﯿﺘﯿﺪه‬ ‫ﻓﺮاﻣﯿﻨﯿﻔﺮﻫﺎي‬ ‫ﭘﻮﺳﺘﻪ‬ ‫ﺷﺪن‬‫ﻣﯽ‬ ‫ﻣﺸﺨﺺ‬ ‫ﯿﺪوﺳﯿﮑﻠﯿﻨﯿﺪه‬‫رﺧﺴﺎره‬ ‫)رﯾﺰ‬ ‫ﺷﻮد‬‫ﻫﺎي‬4O،5O‫و‬6O‫ﺷﺎﻣﻞ‬ ‫دروﻧﯽ‬ ‫رﻣﭗ‬ .(
‫ﺑﺨﺶ‬‫ﻧﯿﻤﻪ‬ ‫ﯾﺎ‬ ‫ﺑﺎز‬ ‫ﻻﮔﻮن‬ ‫ﻫﺎي‬‫ﻣﯽ‬ ‫ﻣﺪي‬ ‫و‬ ‫ﺟﺰر‬ ‫ﭘﻬﻨﻪ‬ ‫و‬ ‫ﻣﺤﺼﻮر‬ ‫ﻻﮔﻮن‬ ،‫ﻣﺤﺼﻮر‬‫رﺧﺴﺎره‬ ‫)رﯾﺰ‬ ‫ﺑﺎز‬ ‫ﻻﮔﻮن‬ ‫ﺷﺮاﯾﻂ‬ ‫در‬ .‫ﺑﺎﺷﺪ‬‫ﻫﺎي‬1L،
2L‫و‬3L‫ﻣﯿﮑﺮوﻓﺴﯿﻞ‬ (‫ﮐﻮراﻟﯿﻨﺎﺳﻪ‬ ‫ﻗﺮﻣﺰ‬ ‫ﺟﻠﺒﮏ‬ ،‫ﻣﻨﻔﺬدار‬ ‫ﻓﺮاﻣﯿﻨﯿﻔﺮﻫﺎي‬ ‫ﻗﺒﯿﻞ‬ ‫از‬ ‫ﻫﺎﯾﯽ‬‫ﺑﺪون‬ ‫ﻓﺮاﻣﯿﻨﯿﻔﺮﻫﺎي‬ ‫ﺑﺎ‬ ‫ﻫﻤﺮاه‬ ‫ﻣﺮﺟﺎن‬ ‫و‬ ‫آ‬‫ﻣﻨﻔﺬ‬
‫رﺧﺴﺎره‬ ‫رﯾﺰ‬ ‫در‬ ‫ﻣﺤﺼﻮر‬ ‫ﻻﮔﻮن‬ ‫در‬ ‫ﭘﺮﺳﻼﻧﻮز‬ ‫ﻓﺮاﻣﯿﻨﯿﻔﺮﻫﺎي‬ ‫ﺗﻨﻮع‬ ‫ﻋﺎﻣﻞ‬ ،‫اﻧﺪك‬ ‫ﺣﺪ‬ ‫در‬ ‫آب‬ ‫ﺗﻼﻃﻢ‬ .‫دارﻧﺪ‬ ‫ﺣﻀﻮر‬4L‫ﻣﺤﺴﻮب‬
‫ﻣﯽ‬‫ﺑﺴﺘﻪ‬ ‫ﺷﺮاﯾﻂ‬ ‫در‬ .‫ﺷﻮد‬‫ﮔﻮﻧﻪ‬ ‫ﺗﻨﻮع‬ ‫آب‬ ‫ﮐﻢ‬ ‫ﺑﺴﯿﺎر‬ ‫ﻫﯿﺪروﻟﯿﮑﯽ‬ ‫اﻧﺮژي‬ ‫ﺷﺮاﯾﻂ‬ ‫ﺑﺎ‬ ،‫ﺗﺮ‬‫ﺑﺎﻓﺖ‬ ‫و‬ ‫ﯾﺎﻓﺘﻪ‬ ‫ﮐﺎﻫﺶ‬ ‫ﭘﺮﺳﻼﻧﻮزي‬ ‫ﻫﺎي‬‫ﮔﻞ‬-
‫ﭘﺸﺘ‬‫ﻣﯽ‬ ‫ﻏﺎﻟﺐ‬ ‫ﯿﺒﺎن‬‫رﺧﺴﺎره‬ ‫)رﯾﺰ‬ ‫ﮔﺮدد‬‫ﻫﺎي‬5L‫و‬6L.(
‫ﺷﮑﻞ‬4-‫ﮔﻮﻧﻪ‬ ‫ﮔﺴﺘﺮش‬ ‫ﻣﺪل‬.‫درﯾﺲ‬ ‫ﺑﺮش‬ ‫در‬ ‫آﺳﻤﺎري‬ ‫ﺳﺎزﻧﺪ‬ ‫اﻟﯿﮕﻮﺳﻦ‬ ‫ﮐﺮﺑﻨﺎﺗﻪ‬ ‫رﻣﭗ‬ ‫در‬ ‫ﻓﺴﯿﻠﯽ‬ ‫ﻫﺎي‬
A: Discorbis sp., Sample no. B267; B: miliolids, Sample no. B440; C: Valvulinid sp., Sample no. B275; D:
Austrotrillina howchini, Sample no., B440, E: Archaias asmaricus, Sample no. B267; F: Peneroplis thomasi,
Sample no. B289; G: Elphidium sp.1, Sample no. B249; H: coralline red algae, Sample no. B313, I: Heterostegina
sp., Sample no. B225; J: coral particle, Sample no. B297; K: Neorotalia viennoti, Sample no. B71; L: coralline
red algae, Sample no. B41; M: Nephrolepidina tournoueri, Sample no. B52; N: Operculina complanata, Sample
no. B27; O: Eulepidina sp., Sample no. B63; P: Nummulites vascus, Sample no. B17; Q: Heterostegina sp.,
Sample no. B0.
4-3-‫ﺑﺮش‬ ‫در‬ ‫آﺳﻤﺎري‬ ‫ﺳﺎزﻧﺪ‬ ‫رﺳﻮﺑﯽ‬ ‫ﻣﺤﯿﻂ‬ ‫و‬ ‫ﺳﻦ‬ ‫ﺗﻄﺎﺑﻖ‬‫و‬ ‫دﯾﻞ‬ ‫ﺗﺎﻗﺪﯾﺲ‬ ،‫ﻧﺎاورا‬ ‫ﺗﺎﻗﺪﯾﺲ‬ ،‫درﯾﺲ‬ ‫ﻫﺎي‬
‫دﻫﻠﺮان‬
‫ﺗﻪ‬ ‫زﻣﺎن‬ ‫در‬ ‫زاﮔﺮس‬ ‫ﻓﻮرﻟﻨﺪ‬ ‫ﺣﻮﺿﻪ‬ ‫ﻧﺴﺒﯽ‬ ‫ﺷﯿﺐ‬ ‫و‬ ‫ﻋﻤﻖ‬ ‫درك‬ ‫ﻣﻨﻈﻮر‬ ‫ﺑﻪ‬‫آﺳﻤﺎري‬ ‫ﺳﺎزﻧﺪ‬ ‫ﻧﺸﺴﺖ‬،‫ﺣﻮﺿﻪ‬ ‫اﯾﻦ‬ ‫ﻣﺨﺘﻠﻒ‬ ‫ﻣﻨﺎﻃﻖ‬ ‫در‬
4،‫ﻫﻤﮑﺎران‬ ‫و‬ ‫)ﺳﻠﻄﺎﻧﯿﺎن‬ ‫ﻧﺎاورا‬ ‫ﺗﺎﻗﺪﯾﺲ‬ ‫ﺑﺮش‬2011‫)اﷲ‬ ‫دﯾﻞ‬ ‫ﺗﺎﻗﺪﯾﺲ‬ ،‫درﯾﺲ‬ ،(‫ﮐﺮم‬،‫ﻫﻤﮑﺎران‬ ‫و‬ ‫دﯾﻞ‬ ‫ﭘﻮر‬2010‫دﻫﻠﺮان‬ ‫و‬ (
‫)وزﯾﺮي‬،‫ﻫﻤﮑﺎران‬ ‫و‬ ‫ﻣﻘﺪم‬2010‫ﻣﺤﯿﻂ‬ ‫و‬ ‫ﺳﻦ‬ ‫ﻧﻈﺮ‬ ‫از‬ (‫ﻣﯽ‬ ‫ﻣﻘﺎﯾﺴﻪ‬ ‫ﻫﻢ‬ ‫ﺑﺎ‬ ‫رﺳﻮﺑﯽ‬ ‫ﻫﺎي‬‫ﺑﺮش‬ .‫ﺷﻮﻧﺪ‬‫اﻣﺘﺪاد‬ ‫ﯾﮏ‬ ‫در‬ ‫ﺷﺪه‬ ‫ذﮐﺮ‬ ‫ﻫﺎي‬
‫ﺟﻨﻮب‬‫ﺷﺮﻗﯽ‬-‫ﺷﻤﺎل‬‫ﺣﺪاﻗﻞ‬ ‫ﻓﻮاﺻﻞ‬ ‫ﺑﺎ‬ ‫ﻏﺮﺑﯽ‬100‫)ﺷﮑﻞ‬ ‫ﻫﺴﺘﻨﺪ‬ ‫واﻗﻊ‬ ‫ﻫﻢ‬ ‫ﺑﻪ‬ ‫ﻧﺴﺒﺖ‬ ‫ﮐﯿﻠﻮﻣﺘﺮي‬5.(

12. ‫رﯾﺰ‬‫رﺧﺴﺎره‬‫ﻫﺎ‬‫و‬‫ﻣﺪل‬‫رﺳﻮﺑﯽ‬‫ﺳﺎزﻧﺪ‬‫آﺳﻤﺎري‬)‫اﻟﯿﮕﻮﺳﻦ‬(‫در‬‫ﺷﻤﺎل‬‫ﻏﺮب‬‫روﺳﺘﺎي‬‫درﯾﺲ‬...
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‫ﻧﺎاورا‬ ‫ﺗﺎﻗﺪﯾﺲ‬ ‫ﺑﺮش‬
‫ﺿﺨﺎﻣﺖ‬ ‫ﺑﺎ‬ ‫ﻧﺎاورا‬ ‫ﺗﺎﻗﺪﯾﺲ‬ ‫ﺑﺮش‬ ‫در‬ ‫آﺳﻤﺎري‬ ‫ﺳﺎزﻧﺪ‬270‫و‬ ‫)ﺳﻠﻄﺎﻧﯿﺎن‬ ‫اﺳﺖ‬ ‫واﻗﻊ‬ ‫زاﮔﺮس‬ ‫ﺣﻮﺿﻪ‬ ‫داﺧﻠﯽ‬ ‫ﻓﺎرس‬ ‫زون‬ ‫در‬ ‫ﻣﺘﺮ‬
،‫ﻫﻤﮑﺎران‬2011‫)ﺷﮑﻞ‬ (6‫ﺑﺨﺶ‬ ‫در‬ ‫ﺑﺮش‬ ‫اﯾﻦ‬ ‫در‬ ‫آﺳﻤﺎري‬ ‫ﺳﺎزﻧﺪ‬ ‫واﻗﻊ‬ ‫در‬ .(‫ﮐﻢ‬ ‫ﻫﺎي‬‫زاﮔﺮس‬ ‫ﻓﻮرﻟﻨﺪ‬ ‫ﺣﻮﺿﻪ‬ ‫ﻟﺒﻪ‬ ‫در‬ ‫و‬ ‫ﻋﻤﻖ‬
‫ﺑﻪ‬ ‫ﭘﺎﺑﺪه‬ ‫ﺳﺎزﻧﺪ‬ ‫ﺑﺎ‬ ‫آﺳﻤﺎري‬ ‫ﺳﺎزﻧﺪ‬ ‫زﯾﺮﯾﻦ‬ ‫ﻣﺮز‬ ‫ﺑﺮش‬ ‫اﯾﻦ‬ ‫در‬ .‫اﺳﺖ‬ ‫ﺷﺪه‬ ‫ﺗﺸﮑﯿﻞ‬‫ﺗﻪ‬ ‫و‬ ‫ﺑﻮده‬ ‫ﭘﯿﻮﺳﺘﻪ‬ ‫ﺻﻮرت‬‫ﺳﺎ‬ ‫ﻧﺸﺴﺖ‬‫آﺳﻤﺎري‬ ‫زﻧﺪ‬
‫رﺧﺴﺎره‬ ‫ﺗﺸﮑﯿﻞ‬ ‫ﺑﺎ‬ ‫روﭘﻠﯿﻦ‬ ‫زﻣﺎن‬ ‫در‬‫ﻣﯽ‬ ‫ﺻﻮرت‬ ‫درﯾﺎﯾﯽ‬ ‫ﻋﻤﯿﻖ‬ ‫ﻫﺎي‬‫رﺧﺴﺎره‬ ‫ﺗﺸﮑﯿﻞ‬ ‫و‬ ‫آب‬ ‫ﻋﻤﻖ‬ ‫ﮐﺎﻫﺶ‬ ‫ﺑﺎ‬ .‫ﮔﯿﺮد‬‫ﻻ‬ ‫ﻣﺤﯿﻂ‬ ‫ﻫﺎي‬‫ﮔﻮن‬
‫ﺷﺎﺗﯿ‬ ‫زﻣﺎن‬ ‫در‬‫ﺗﻪ‬ ‫ﺳﺮاﻧﺠﺎم‬ ،‫ﻦ‬‫ﻣﯽ‬ ‫اﺗﻤﺎم‬ ‫ﺑﻪ‬ ‫آﺳﻤﺎري‬ ‫ﺳﺎزﻧﺪ‬ ‫ﻧﺸﺴﺖ‬‫ﺗﻪ‬ ،‫ﻧﺎﺣﯿﻪ‬ ‫اﯾﻦ‬ ‫در‬ ‫زاﮔﺮس‬ ‫ﺣﻮﺿﻪ‬ ‫ﮐﻢ‬ ‫ﻋﻤﻖ‬ ‫دﻟﯿﻞ‬ ‫ﺑﻪ‬ ‫و‬ ‫رﺳﺪ‬‫ﻧ‬‫ﺸﺴﺖ‬
‫ﻣﯽ‬ ‫ﺷﺮوع‬ ‫ﺷﺎﺗﯿﻦ‬ ‫زﻣﺎن‬ ‫در‬ ‫ﮔﭽﺴﺎران‬ ‫ﺳﺎزﻧﺪ‬ ‫رﺳﻮﺑﺎت‬.‫ﺷﻮد‬
‫درﯾﺲ‬ ‫ﺑﺮش‬
‫ﺿﺨﺎﻣﺖ‬ ‫ﺑﺎ‬ ‫درﯾﺲ‬ ‫ﺑﺮش‬460‫)ﺷﮑﻞ‬ ‫دارد‬ ‫ﻗﺮار‬ ‫داﺧﻠﯽ‬ ‫ﻓﺎرس‬ ‫زون‬ ‫در‬ ‫ﻣﺘﺮ‬6‫در‬ ‫آﺳﻤﺎري‬ ‫ﺳﺎزﻧﺪ‬ ‫ﻓﻮﻗﺎﻧﯽ‬ ‫و‬ ‫ﺗﺤﺘﺎﻧﯽ‬ ‫ﻣﺮزﻫﺎي‬ .(‫اﯾﻦ‬
‫ﺑﻪ‬ ‫ﺑﺮش‬‫ﻣﯽ‬ ‫ﭘﻮﺷﯿﺪه‬ ‫ﺻﻮرت‬‫)روﭘﻠﯿﻦ‬ ‫اﻟﯿﮕﻮﺳﻦ‬ ‫ﻣﻌﺎدل‬ ‫درﯾﺲ‬ ‫ﺑﺮش‬ ‫در‬ ‫آﺳﻤﺎري‬ ‫ﺳﺎزﻧﺪ‬ ‫ﺳﻦ‬ .‫ﺑﺎﺷﺪ‬-‫ﮐ‬ ‫ﻫﻤﺎﻧﮕﻮﻧﻪ‬ .‫اﺳﺖ‬ (‫ﺷﺎﺗﯿﻦ‬‫ﻪ‬
‫رﺧﺴﺎره‬ ‫رﯾﺰ‬ ‫ﺑﺨﺶ‬ ‫در‬‫ﮔﻮﻧﻪ‬ ‫ﺷﺎﻣﻞ‬ ‫ﮐﻪ‬ ‫آﺳﻤﺎري‬ ‫ﺳﺎزﻧﺪ‬ ‫روﭘﻠﯿﻦ‬ ‫رﺳﻮﺑﺎت‬ ،‫اﺳﺖ‬ ‫ﺷﺪه‬ ‫ذﮐﺮ‬ ‫ﻫﺎ‬‫ﻣﯽ‬ ‫ﻧﻮﻣﻮﻟﯿﺘﺲ‬ ‫ﺟﻨﺲ‬ ‫ﻫﺎي‬‫د‬ ،‫ﺑﺎﺷﺪ‬‫ر‬
‫ﺑﺨﺶ‬‫ﻋﻤﯿﻖ‬ ‫ﻫﺎي‬‫ﺷﺪه‬ ‫ﺗﺸﮑﯿﻞ‬ ‫ﻣﯿﺎﻧﯽ‬ ‫رﻣﭗ‬ ‫ﺗﺮ‬‫ﮐﺎ‬ ‫ﺑﺎ‬ .‫اﻧﺪ‬‫ﻣﺤﯿﻂ‬ ‫در‬ ‫ﺑﺮش‬ ‫اﯾﻦ‬ ‫ﺷﺎﺗﯿﻦ‬ ‫رﺳﻮﺑﺎت‬ ،‫آب‬ ‫ﻋﻤﻖ‬ ‫ﻫﺶ‬‫ﺳ‬ ،‫ﻣﯿﺎﻧﯽ‬ ‫رﻣﭗ‬ ‫ﻫﺎي‬،‫ﺪ‬
‫ﻧﯿﻤﻪ‬ ‫ﻻﮔﻮن‬‫ﺗﻪ‬ ‫ﻣﺪي‬ ‫و‬ ‫ﺟﺰر‬ ‫ﭘﻬﻨﻪ‬ ‫و‬ ‫ﻣﺤﺼﻮر‬ ‫ﻻﮔﻮن‬ ،‫ﻣﺤﺼﻮر‬.‫اﺳﺖ‬ ‫ﺷﺪه‬ ‫ﻧﺸﯿﻦ‬
‫دﯾﻞ‬ ‫ﺗﺎﻗﺪﯾﺲ‬ ‫ﺑﺮش‬
‫ﺿﺨﺎﻣﺖ‬ ‫ﺑﺎ‬ ‫دﯾﻞ‬ ‫ﺗﺎﻗﺪﯾﺲ‬ ‫ﺑﺮش‬206‫)اﷲ‬ ‫اﺳﺖ‬ ‫واﻗﻊ‬ ‫اﯾﺬه‬ ‫زون‬ ‫در‬ ‫ﻣﺘﺮ‬‫ﮐﺮم‬،‫ﻫﻤﮑﺎران‬ ‫و‬ ‫دﯾﻞ‬ ‫ﭘﻮر‬2010‫)ﺷﮑﻞ‬ (6‫ﻧﺎﺣﯿﻪ‬ ‫اﯾﻦ‬ ‫در‬ .(
‫زﻣﺎن‬ ‫در‬‫رﺳﻮب‬ ‫و‬ ‫ﺗﺸﮑﯿﻞ‬ ‫ﭘﺎﺑﺪه‬ ‫ﺳﺎزﻧﺪ‬ ‫روﭘﻠﯿﻦ‬‫ﻣﯽ‬ ‫آﻏﺎز‬ ‫ﺷﺎﺗﯿﻦ‬ ‫زﻣﺎن‬ ‫از‬ ‫آﺳﻤﺎري‬ ‫ﺳﺎزﻧﺪ‬ ‫ﮔﺬاري‬‫زﻣﺎن‬ ‫در‬ ‫ﺑﺮش‬ ‫اﯾﻦ‬ ‫ﺑﻨﺎﺑﺮاﯾﻦ‬ .‫ﺷﻮد‬
‫ﻋﻤﯿﻖ‬ ‫ﻧﻮاﺣﯽ‬ ‫در‬ ‫روﭘﻠﯿﻦ‬‫ﺑﺮش‬ ‫ﺑﻪ‬ ‫ﻧﺴﺒﺖ‬ ‫زاﮔﺮس‬ ‫ﻓﻮرﻟﻨﺪ‬ ‫ﺣﻮﺿﻪ‬ ‫از‬ ‫ﺗﺮي‬‫ﻃﺮﻓﯽ‬ ‫از‬ .‫اﺳﺖ‬ ‫داﺷﺘﻪ‬ ‫ﻗﺮار‬ ‫درﯾﺲ‬ ‫و‬ ‫ﻧﺎاورا‬ ‫ﺗﺎﻗﺪﯾﺲ‬ ‫ﻫﺎي‬
‫ﺗﻪ‬ ‫اداﻣﻪ‬‫ﻻﮔﻮ‬ ‫ﻣﺤﯿﻂ‬ ‫در‬ ‫آﺳﻤﺎري‬ ‫ﺳﺎزﻧﺪ‬ ‫رﺳﻮﺑﺎت‬ ‫ﻧﺸﺴﺖ‬‫ﺑﯿﺶ‬ ‫ﻋﻤﻖ‬ ‫ﮐﻨﻨﺪه‬ ‫ﺗﺄﯾﯿﺪ‬ ‫ﻧﯿﺰ‬ ‫ﺑﻮردﯾﮕﺎﻟﯿﻦ‬ ‫ﺳﻦ‬ ‫ﺗﺎ‬ ،‫ن‬‫ﺑﺮ‬ ‫اﯾﻦ‬ ‫ﺗﺮ‬‫ﺑﻪ‬ ‫ﻧﺴﺒﺖ‬ ‫ش‬
‫ﻣﯽ‬ ‫ﻗﺒﻠﯽ‬ ‫ﺑﺮش‬ ‫دو‬‫ﺑﻪ‬ ‫ﮔﭽﺴﺎران‬ ‫ﺳﺎزﻧﺪ‬ ‫ﺑﺎ‬ ‫ﺑﺮش‬ ‫اﯾﻦ‬ ‫ﻓﻮﻗﺎﻧﯽ‬ ‫ﻣﺮز‬ .‫ﺑﺎﺷﺪ‬.‫اﺳﺖ‬ ‫ﭘﯿﻮﺳﺘﻪ‬ ‫ﺻﻮرت‬
‫دﻫﻠﺮان‬ ‫ﺑﺮش‬
‫ﺿﺨﺎﻣﺖ‬ ‫داراي‬ ‫دﻫﻠﺮان‬ ‫ﺑﺮش‬ ‫در‬ ‫آﺳﻤﺎري‬ ‫ﺳﺎزﻧﺪ‬180‫ﻣﯽ‬ ‫ﻣﺘﺮ‬‫)وزﯾﺮي‬ ‫ﺑﺎﺷﺪ‬،‫ﻫﻤﮑﺎران‬ ‫و‬ ‫ﻣﻘﺪم‬2010‫)ﺷﮑﻞ‬ (6‫در‬ ‫ﺑﺮش‬ ‫اﯾﻦ‬ .(
‫ز‬‫ﺗﻪ‬ .‫اﺳﺖ‬ ‫واﻗﻊ‬ ‫زاﮔﺮس‬ ‫ﺣﻮﺿﻪ‬ ‫ﻟﺮﺳﺘﺎن‬ ‫ون‬‫زﻣﺎن‬ ‫اﯾﻦ‬ ‫در‬ ‫رﺳﻮﺑﯽ‬ ‫ﻣﺤﯿﻂ‬ ‫زﯾﺎد‬ ‫ﻋﻤﻖ‬ ‫از‬ ‫ﺣﺎﮐﯽ‬ ‫ﺷﺎﺗﯿﻦ‬ ‫اواﺧﺮ‬ ‫ﺗﺎ‬ ‫ﭘﺎﺑﺪه‬ ‫ﺳﺎزﻧﺪ‬ ‫ﻧﺸﺴﺖ‬
‫ﻣﯽ‬‫ﺗﻪ‬ ‫ﺑﺮش‬ ‫اﯾﻦ‬ ‫در‬ .‫ﺑﺎﺷﺪ‬‫آﮐﯽ‬ ‫زﻣﺎن‬ ‫از‬ ‫ﻻﮔﻮن‬ ‫ﻣﺤﯿﻂ‬ ‫در‬ ‫آﺳﻤﺎري‬ ‫ﺳﺎزﻧﺪ‬ ‫ﻧﺸﺴﺖ‬‫ﻣﯽ‬ ‫اداﻣﻪ‬ ‫ﺑﻮردﯾﮕﺎﻟﯿﻦ‬ ‫ﺗﺎ‬ ‫و‬ ‫ﺷﺪه‬ ‫ﺷﺮوع‬ ‫ﺗﺎﻧﯿﻦ‬‫ﯾ‬.‫ﺎﺑﺪ‬
‫رﺳﻮب‬ ‫ﻫﻤﭽﻨﯿﻦ‬‫رو‬ ‫ﺑﺮ‬ ‫ﮔﭽﺴﺎران‬ ‫ﺳﺎزﻧﺪ‬ ‫ﮔﺬاري‬‫ﻣﯽ‬ ‫ﺷﺮوع‬ ‫ﺑﻮردﯾﮕﺎﻟﻦ‬ ‫ﺳﻦ‬ ‫در‬ ‫آﺳﻤﺎري‬ ‫ﺳﺎزﻧﺪ‬ ‫ي‬‫رﺳﻮﺑﺎت‬ ‫ﺿﺨﺎﻣﺖ‬ .‫ﺷﻮد‬
‫ﺑﯿﺶ‬ ‫دﯾﻞ‬ ‫ﺗﺎﻗﺪﯾﺲ‬ ‫ﺑﺮش‬ ‫ﺑﻪ‬ ‫ﻧﺴﺒﺖ‬ ‫ﺑﺮش‬ ‫اﯾﻦ‬ ‫در‬ ‫آﺳﻤﺎري‬ ‫ﺳﺎزﻧﺪ‬ ‫ﺑﻮردﯾﮕﺎﻟﯿﻦ‬‫ﻣﯽ‬ ‫ﺗﺮ‬‫ﻋﻤﯿﻖ‬ ‫در‬ ‫ﺑﺮش‬ ‫اﯾﻦ‬ ً‫ﻻ‬‫اﺣﺘﻤﺎ‬ .‫ﺑﺎﺷﺪ‬‫ﺗ‬‫ﺮﯾﻦ‬
‫ﺑﺨﺶ‬‫ﺑﻪ‬ ‫اﺳﺖ؛‬ ‫داﺷﺘﻪ‬ ‫ﻗﺮار‬ ‫زاﮔﺮس‬ ‫ﻓﻮرﻟﻨﺪ‬ ‫ﺣﻮﺿﻪ‬ ‫ﻫﺎي‬‫ﻃﻮري‬‫ﺗﻪ‬ ‫ﮐﻪ‬‫ﺑﺮش‬ ‫اﯾﻦ‬ ‫در‬ ‫آﺳﻤﺎري‬ ‫ﺳﺎزﻧﺪ‬ ‫رﺳﻮﺑﺎت‬ ‫ﻧﺸﺴﺖ‬‫ﻧﺴﺒﺖ‬‫ﺑﻪ‬
‫ﺑﺮش‬‫ﺟﻮان‬ ‫زﻣﺎن‬ ‫در‬ ،‫دﯾﻞ‬ ‫ﺗﺎﻗﺪﯾﺲ‬ ‫و‬ ‫درﯾﺲ‬ ،‫ﻧﺎاورا‬ ‫ﺗﺎﻗﺪﯾﺲ‬ ‫ﻫﺎي‬.‫اﺳﺖ‬ ‫اﻓﺘﺎده‬ ‫اﺗﻔﺎق‬ ‫ﺗﺮي‬

13. ‫رﯾﺰ‬‫رﺧﺴﺎره‬‫ﻫﺎ‬‫و‬‫ﻣﺪل‬‫رﺳﻮﺑﯽ‬‫ﺳﺎزﻧﺪ‬‫آﺳﻤﺎري‬)‫اﻟﯿﮕﻮﺳﻦ‬(‫در‬‫ﺷﻤﺎل‬‫ﻏﺮب‬‫روﺳﺘﺎي‬‫درﯾﺲ‬...
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‫ﺷﮑﻞ‬5-‫ﺑﺮش‬ ‫ﻣﻮﻗﻌﯿﺖ‬‫زون‬ ‫ﺑﻪ‬ ‫ﺗﻮﺟﻪ‬ ‫ﺑﺎ‬ ‫ﺗﻄﺎﺑﻖ‬ ‫ﻣﻮرد‬ ‫ﻫﺎي‬‫)ﻓﺮﺿﯽ‬ ‫زاﮔﺮس‬ ‫ﺣﻮﺿﻪ‬ ‫ﺳﺎﺧﺘﺎري‬ ‫ﻫﺎي‬‫ﭘﻮر‬-،‫ﻫﻤﮑﺎران‬ ‫و‬ ‫ﺳﺎﺋﯿﻦ‬2009.(
5‫ﻧﺘ‬ .‫ﯿ‬‫ﮔ‬ ‫ﺠﻪ‬‫ﯿ‬‫ﺮ‬‫ي‬
‫در‬ ‫و‬ ‫درﯾﺲ‬ ‫روﺳﺘﺎي‬ ‫ﺣﻮاﻟﯽ‬ ‫در‬ ‫ﻣﻄﺎﻟﻌﻪ‬ ‫ﻣﻮرد‬ ‫ﺑﺮش‬7‫ﻣﻮﻗﻌﯿﺖ‬ .‫اﺳﺖ‬ ‫ﺷﺪه‬ ‫واﻗﻊ‬ ‫ﮐﺎزرون‬ ‫ﺷﻬﺮﺳﺘﺎن‬ ‫ﻏﺮب‬ ‫ﺷﻤﺎل‬ ‫ﮐﯿﻠﻮﻣﺘﺮي‬
‫ﺑﺮش‬ ‫اﯾﻦ‬ ‫ﺟﻐﺮاﻓﯿﺎﯾﯽ‬''26'32o
51‫و‬ ‫ﺷﺮﻗﯽ‬''59'41o
29‫ﻣﯽ‬ ‫ﺷﻤﺎﻟﯽ‬‫ﺑﺎﺷﺪ‬‫ﺿﺨﺎﻣﺖ‬ ‫داراي‬ ‫درﯾﺲ‬ ‫ﺑﺮش‬ ‫در‬ ‫آﺳﻤﺎري‬ ‫ﺳﺎزﻧﺪ‬ .
460،‫ﻧﺎزك‬ ‫ﺧﺎﮐﺴﺘﺮي‬ ‫ﺑﻪ‬ ‫ﻣﺘﻤﺎﯾﻞ‬ ‫ﮐﺮم‬ ‫ﺗﺎ‬ ‫ﺧﺎﮐﺴﺘﺮي‬ ‫آﻫﮏ‬ ‫ﻣﺘﺮ‬‫ﻻﯾﻪ‬ ‫ﻣﯿﺎن‬ ‫ﺑﺎ‬ ‫دوﻟﻮﻣﯿﺘﯽ‬ ً‫ﺎ‬‫ﺑﻌﻀ‬ ‫و‬ ‫ﻣﺎﺳﯿﻮ‬ ،‫ﺿﺨﯿﻢ‬ ،‫ﻣﺘﻮﺳﻂ‬‫ﻫ‬‫ﻧﻮدوﻻر‬ ‫ﺎي‬
‫ﻣﯽ‬ ‫ﻣﺎرﻧﯽ‬ ‫و‬‫ﻻﯾﻪ‬ ‫ﺿﺨﺎﻣﺖ‬ ‫ﺑﻪ‬ ‫ﺗﻮﺟﻪ‬ ‫ﺑﺎ‬ ‫و‬ ‫ﺻﺤﺮاﯾﯽ‬ ‫ﻣﻄﺎﻟﻌﺎت‬ ‫اﺳﺎس‬ ‫ﺑﺮ‬ ‫ﮐﻪ‬ ‫ﺑﺎﺷﺪ‬‫ﻓﺴﯿﻠﯽ‬ ‫آﺛﺎر‬ ‫و‬ ‫رﻧﮓ‬ ،‫ﻟﯿﺘﻮﻟﻮژي‬ ،‫ﻫﺎ‬5‫ﺳﻨﮓ‬ ‫واﺣﺪ‬‫ﭼﯿﻨﻪ‬
‫)روﭘ‬ ‫اﻟﯿﮕﻮﺳﻦ‬ ‫ﻣﻌﺎدل‬ ‫ﺑﺮش‬ ‫اﯾﻦ‬ ‫در‬ ‫آﺳﻤﺎري‬ ‫ﺳﺎزﻧﺪ‬ ‫ﺳﻦ‬ .‫اﺳﺖ‬ ‫ﮔﺸﺘﻪ‬ ‫ﻣﻌﺮﻓﯽ‬ ‫ﻣﺬﮐﻮر‬ ‫ﺑﺮش‬ ‫ﺑﺮاي‬ ‫ﻧﮕﺎري‬‫ﻠﯿﻦ‬-‫ﻣﯽ‬ (‫ﺷﺎﺗﯿﻦ‬‫ﺑ‬.‫ﺎﺷﺪ‬‫ﭘﺲ‬
‫ﻣﺠﻤﻮع‬ ‫در‬ ،‫ﻣﯿﮑﺮوﺳﮑﻮﭘﯽ‬ ‫ﻧﺎزك‬ ‫ﻣﻘﺎﻃﻊ‬ ‫ﺑﺮرﺳﯽ‬ ‫و‬ ‫ﺻﺤﺮاﯾﯽ‬ ‫ﻣﻄﺎﻟﻌﺎت‬ ‫از‬14‫و‬ ‫رﺧﺴﺎره‬ ‫رﯾﺰ‬4‫ﺑﺮاي‬ ‫رﺳﻮﺑﯽ‬ ‫رﺧﺴﺎره‬ ‫رﯾﺰ‬ ‫زﯾﺮ‬
‫ﺑﻪ‬ ‫ﺳﺎزﻧﺪ‬ ‫اﯾﻦ‬ ‫رﺳﻮﺑﯽ‬ ‫ﻣﺤﯿﻂ‬ ‫و‬ ،‫ﻣﻌﺮﻓﯽ‬ ‫آﺳﻤﺎري‬ ‫ﺳﺎزﻧﺪ‬‫ﻣﯽ‬ ‫ﮔﺮﻓﺘﻪ‬ ‫ﻧﻈﺮ‬ ‫در‬ ‫ﻫﻤﻮﮐﻠﯿﻨﺎل‬ ‫رﻣﭗ‬ ‫ﯾﮏ‬ ‫ﺻﻮرت‬‫رﺳﻮﺑ‬ ‫ﻣﺤﯿﻂ‬ ‫اﯾﻦ‬ .‫ﺷﻮد‬‫ﯽ‬
‫دروﻧﯽ‬ ‫رﻣﭗ‬ ‫و‬ ‫ﻣﯿﺎﻧﯽ‬ ‫رﻣﭗ‬ ‫ﺷﺎﻣﻞ‬‫رﺧﺴﺎره‬ ‫وﺟﻮد‬ ‫ﻋﺪم‬ ‫دﻟﯿﻞ‬ ‫ﺑﻪ‬ ‫و‬ ‫ﺑﻮده‬‫ﻣﺤﯿﻂ‬ ‫اﯾﻦ‬ ‫ﺑﺮاي‬ ‫ﺑﯿﺮوﻧﯽ‬ ‫رﻣﭗ‬ ،‫درﯾﺎﯾﯽ‬ ‫ﻋﻤﯿﻖ‬ ‫ﻣﺤﯿﻂ‬ ‫ﻫﺎي‬
‫ﻧﻤﯽ‬ ‫ﻣﻌﺮﻓﯽ‬ ‫رﺳﻮﺑﯽ‬‫در‬ ‫آﺳﻤﺎري‬ ‫ﺳﺎزﻧﺪ‬ ‫ﺗﻄﺎﺑﻖ‬ ‫ﺑﺎ‬ ‫ﻫﻤﭽﻨﯿﻦ‬ .‫ﮔﺮدد‬4‫در‬ ،‫دﻫﻠﺮان‬ ‫و‬ ‫دﯾﻞ‬ ‫ﺗﺎﻗﺪﯾﺲ‬ ،‫درﯾﺲ‬ ،‫ﻧﺎاورا‬ ‫ﺗﺎﻗﺪﯾﺲ‬ ‫ﺑﺮش‬
‫ﺟﻨﻮب‬ ‫اﻣﺘﺪاد‬‫ﺷﺮﻗﯽ‬-‫ﺷﻤﺎل‬‫ﺟﻮان‬ ،‫ﻏﺮﺑﯽ‬‫ﺑﻪ‬ ‫آﺳﻤﺎري‬ ‫ﺳﺎزﻧﺪ‬ ‫رأس‬ ‫و‬ ‫ﻗﺎﻋﺪه‬ ‫ﺳﻦ‬ ‫ﺷﺪن‬ ‫ﺗﺮ‬‫ﺑﺨﺶ‬ ‫ﺳﻤﺖ‬‫ﻋﻤﯿﻖ‬ ‫ﻫﺎي‬‫ﻓﻮرﻟﻨﺪ‬ ‫ﺣﻮﺿﻪ‬ ‫ﺗﺮ‬
‫ﻣﯽ‬ ‫ﺗﺄﯾﯿﺪ‬ ‫زاﮔﺮس‬.‫ﺷﻮد‬

14. ‫رﯾﺰ‬‫رﺧﺴﺎره‬‫ﻫﺎ‬‫و‬‫ﻣﺪل‬‫رﺳﻮﺑﯽ‬‫ﺳﺎزﻧﺪ‬‫آﺳﻤﺎري‬)‫اﻟﯿﮕﻮﺳﻦ‬(‫در‬‫ﺷﻤﺎل‬‫ﻏﺮب‬‫روﺳﺘﺎي‬‫درﯾﺲ‬...
١٤
‫ﺷﮑﻞ‬6-‫ﻣﺤﯿﻂ‬ ‫و‬ ‫ﺳﻦ‬ ،‫ﺿﺨﺎﻣﺖ‬ ‫ﻣﻘﺎﯾﺴﻪ‬‫ﺑﺮش‬ ‫رﺳﻮﺑﯽ‬ ‫ﻫﺎي‬‫)ﺟﻮان‬ ‫ﺗﻄﺎﺑﻖ‬ ‫ﻣﻮرد‬ ‫ﻫﺎي‬‫ﺟﻨﻮب‬ ‫از‬ ‫آﺳﻤﺎري‬ ‫ﺳﺎزﻧﺪ‬ ‫ﺷﺪن‬ ‫ﺗﺮ‬‫ﺳﻤﺖ‬ ‫ﺑﻪ‬ ‫ﺷﺮق‬‫ﺷﻤﺎل‬-
‫ﺑﺮش‬ ‫ﻣﺤﻞ‬ ‫و‬ ‫ﻣﺄﺧﺬ‬ ‫ﻧﻘﺸﻪ‬ ‫ﻣﺸﺎﻫﺪه‬ ‫ﺑﺮاي‬ .(‫ﻏﺮب‬‫ﺷﮑﻞ‬ ‫ﺑﻪ‬ ‫ﻫﺎ‬5.‫ﺷﻮد‬ ‫ﻣﺮاﺟﻌﻪ‬
‫ﻗﺪرداﻧ‬ ‫و‬ ‫ﺗﺸﮑﺮ‬‫ﯽ‬
‫از‬‫داوران‬‫آﻗﺎﯾﺎن‬ ‫ﻣﻘﺎﻟﻪ‬‫دﮐﺘﺮ‬‫رﺣﻤﺎﻧﯽ‬‫و‬‫دﮐﺘﺮ‬‫ﺻﻔﺮي‬‫ﺑﻪ‬‫ﺧﺎﻃﺮ‬‫ﻧﻈﺮات‬‫ﻣﻮﺛﺮ‬‫و‬‫ﺳﺎزﻧﺪه‬‫در‬‫ﺟﻬﺖ‬‫ﭘ‬‫ﯿ‬‫ﺸﺒﺮد‬‫دﺳﺘﺎوردﻫﺎ‬‫ي‬‫ا‬‫ﯾ‬‫ﻦ‬‫ﭘ‬‫ﮋوﻫﺶ‬
‫ﻫﻤﭽﻨﯿﻦ‬ ‫و‬‫از‬‫داﻧﺸﮕﺎه‬‫اﺻﻔﻬﺎن‬‫ﺑﻪ‬‫ﺧﺎﻃﺮ‬‫ﺣﻤﺎﯾﺖ‬‫ﻫﺎي‬‫ﻣﺎﻟﯽ‬‫و‬‫در‬‫اﺧﺘﯿﺎر‬‫ﮔﺬاﺷﺘﻦ‬‫اﻣﮑﺎﻧﺎت‬‫ﻻزم‬‫ﺑﺮاي‬‫ﺗﺤﻘﯿﻖ‬ ‫اﯾﻦ‬‫ﺗﺸﮑﺮ‬‫ﺑ‬‫ﻋﻤﻞ‬ ‫ﻪ‬
.‫آﯾﺪ‬ ‫ﻣﯽ‬

15. ‫رﯾﺰ‬‫رﺧﺴﺎره‬‫ﻫﺎ‬‫و‬‫ﻣﺪل‬‫رﺳﻮﺑﯽ‬‫ﺳﺎزﻧﺪ‬‫آﺳﻤﺎري‬)‫اﻟﯿﮕﻮﺳﻦ‬(‫در‬‫ﺷﻤﺎل‬‫ﻏﺮب‬‫روﺳﺘﺎي‬‫درﯾﺲ‬...
١٥
6.‫ﻣﻨﺎﺑﻊ‬
-،‫ﺻﯿﺮﻓﯿﺎن‬ ،.‫س‬ ،‫اﺧﺰري‬.‫ع‬،‫و‬‫وزﯾﺮي‬‫ﻣﻘﺪم‬،‫ح‬.،1394‫زﯾﺴﺖ‬ ،‫ﭼﯿﻨﻪ‬‫ﺷﻤﺎل‬ ‫در‬ ‫آﺳﻤﺎري‬ ‫ﺳﺎزﻧﺪ‬ ‫ﻧﮕﺎري‬‫اﺳﺘﺎن‬ ‫)ﻏﺮب‬ ‫درﯾﺲ‬ ‫روﺳﺘﺎي‬ ‫ﻏﺮب‬
‫دﯾﺮﯾﻨﻪ‬ ‫اﻧﺠﻤﻦ‬ ‫ﻫﻤﺎﯾﺶ‬ ‫ﻧﻬﻤﯿﻦ‬ :(‫ﻓﺎرس‬‫ص‬ ،‫اﯾﺮان‬ ‫ﺷﻨﺎﺳﯽ‬11-7.
-،.‫ع‬ ،‫آﻗﺎﻧﺒﺎﺗﯽ‬1383‫زﻣﯿﻦ‬ ،‫زﻣﯿﻦ‬ ‫ﺳﺎزﻣﺎن‬ ‫اﻧﺘﺸﺎرات‬ :‫اﯾﺮان‬ ‫ﺷﻨﺎﺳﯽ‬،‫ﻣﻌﺪﻧﯽ‬ ‫اﮐﺘﺸﺎف‬ ‫و‬ ‫ﺷﻨﺎﺳﯽ‬586.‫ﺻﻔﺤﻪ‬
-‫ﺟﻐﺮاﻓﯿﺎﯾﯽ‬ ‫ﺳﺎزﻣﺎن‬،‫ﻣﺴﻠﺢ‬ ‫ﻧﯿﺮوﻫﺎي‬1384‫ﻣﻘﯿﺎس‬ ،‫ﺗﻬﺮان‬ :‫اﯾﺮان‬ ‫اﺳﻼﻣﯽ‬ ‫ﺟﻤﻬﻮري‬ ‫ﮐﺸﻮر‬ ‫ﻧﻘﺸﻪ‬ ،1:2000000.
-‫دروﯾﺶ‬،.‫ع‬ ،‫زاده‬1388‫زﻣﯿﻦ‬ ،‫ﭼﯿﻨﻪ‬ ‫اﯾﺮان‬ ‫ﺷﻨﺎﺳﯽ‬،‫اﻣﯿﺮﮐﺒﯿﺮ‬ ‫اﻧﺘﺸﺎرات‬ ‫ﻣﻮﺳﺴﻪ‬ ،‫ﺗﻬﺮان‬ :‫ﻣﺎﮔﻤﺎﺗﯿﺴﻢ‬ ‫و‬ ‫دﮔﺮﮔﻮﻧﯽ‬ ،‫ﺗﮑﺘﻮﻧﯿﮏ‬ ،‫ﺷﻨﺎﺳﯽ‬434
.‫ﺻﻔﺤﻪ‬
-،.‫ع‬ ،‫ﺻﯿﺮﻓﯿﺎن‬1386‫زﻣﯿﻦ‬ ،،‫ﺳﻤﺮ‬ ‫اﻧﺘﺸﺎرات‬ :‫ﻧﻔﺖ‬ ‫ﺷﻨﺎﺳﯽ‬373‫ﺻ‬.‫ﻔﺤﻪ‬
-،.‫ه‬ ،‫ﻣﻄﯿﻌﯽ‬1372‫زﻣﯿﻦ‬ ،‫)ﭼﯿﻨﻪ‬ ‫اﯾﺮان‬ ‫ﺷﻨﺎﺳﯽ‬‫زﻣﯿﻦ‬ ‫ﺳﺎزﻣﺎن‬ ‫اﻧﺘﺸﺎرات‬ :(‫زاﮔﺮس‬ ‫ﺷﻨﺎﺳﯽ‬،‫ﺷﻨﺎﺳﯽ‬538.‫ﺻﻔﺤﻪ‬
-ADABI, M.H., RAO, C.P., and KITTO, P.A., 1996, The source of hydrothermal fluids responsible for
carbonate alteration, Renison, Tasmania, Australia: 13th Geol. Conv. Australia, (abst.), 41, 7.
-ALAVI, M., 2004, Regional stratigraphy of the Zagros fold-thrust belt of Iran and its proforeland evolution:
American Journal of Science, 304, 1-20.
-ALLAHKARAMPOUR DILL, M., SEYRAFIAN, A., and VAZIRI-MOGHADAM, H., 2010, The Asmari
Formation, north of the Gachsaran (Dill anticline), southwest Iran, facies analysis, depositional environments
and sequence stratigraphy: Carbonate and Evaporites, 25(2), 145-160.
-BARATTOLO, F., BASSI, D., and ROMERO, R., 2007, Upper Eocene larger foraminifera coralline algae
facies from the Klokova Mountain (south continental Greece): Facies, 53(3), 361-375.
-DANIEL, J.M., NADER, F., HAMON, J.Y., and CALLOT, J.P., 2008, Asmari Reservoir Modeling-Field Scale
Study of Gachsaran-Final Report Part1: The international IOR research cooperation for Iranian fields, Joint
Study Program, Tehran, Iran.
-DUNHAM, R.J., 1962, Classification of carbonate rocks according to their depositional texture, in W. E., Ham,
ed., Classification of carbonate rocks. American Association of Petroleum Geologists Memoir, 1, 108-121.
-EMBRY, A.F., and Klovan, J.E., 1971, Late Devonian reef tract on northeastern Banks Island, Northwest
territories: Bulletin of Canadian Petroleum Geology, 19, 730-781.
-FARZIPOUR-SAEIN, A., YASSAGHI, A., SHERKATI, S., and KOYI, H., 2009, Basin evolution of the
Lurestan region in the Zagros fold and thrust belt, Iran: Journal of Petroleum Geology, 32, 5-19.
-FLUGEL, E., 2010, Microfacies of Carbonate Rocks. Springer, 984.
-GEEL, H., 2000, Recognition of stratigraphic carbonate platform and slope deposits: empirical models based
on microfacies analysis of paleogene deposits in southeastern Spain: Paleogeography, Paleoclimatology,
Paleoecology, 1550, 211-238.
-LAURSEN, G.V., MONIBI, S., ALLAN, T.L., PICKARD, N.A.H., HOSSEINEY, A., VINCENT, B.,
HAMON, Y., VAN BUCHEM, F.S.P., MOALLEMI, A., and DRUILLION, G., 2009, The Asmari Formation
revisited: changed stratigraphic allocation and new biozonation: First International Petroleum Conference and
Exhibition, Shiraz, Iran.
-MACLEOD, J.H., and MAJEDI, M., 1972, Geological compilation map of Kazerun: Tehran, Geological and
Exploration Division, 25484, 1: 100000, sheet no. 20846 E.
-NEBELSICK, J., and BASSI, D., 2000, Diversity, growthforms and taphonomy: key factors controlling the
fabric of coralline algae dominated shelf carbonates.in E. insalaco, P. Skelton, and T, Palmer, eds., Carbonate
platform systems. Compounents and interactions: Geological Society, London, 178, 89-107.

16. ‫رﯾﺰ‬‫رﺧﺴﺎره‬‫ﻫﺎ‬‫و‬‫ﻣﺪل‬‫رﺳﻮﺑﯽ‬‫ﺳﺎزﻧﺪ‬‫آﺳﻤﺎري‬)‫اﻟﯿﮕﻮﺳﻦ‬(‫در‬‫ﺷﻤﺎل‬‫ﻏﺮب‬‫روﺳﺘﺎي‬‫درﯾﺲ‬...
١٦
-POMAR, L., 2001, Types of carbonate platforms: A genetic approach, Basin Research, 13, 313-334.
-ROMERO, J., CAUS., E., and ROSSEL, J., 2002, A model for the paleoenvironmental distribiution of larger
foraminifera based on late Eocene deposit on the margine of the south Pyrenean basin (SE Spain):
Palaeogeography, Palaeoclimetology, Palaeoecology, 179, 43-56.
-SADEGHI, R., VAZIRI-MOGHADDAM, H., and TAHERI, A., 2009, Biostratigraphy and paleoecology of
the Oligo-Miocene succession in Fars and Khuzestan areas (Zagros Basin, SW Iran): Historical Biology, 21(2),
17-31.
-SADEGHI, R., VAZIRI-MOGHADDAM, H., and TAHERI, A., 2010, Microfacies and sedimentary
environment of the Oligocene sequence (Asmari Formation) in Fars sub-basin, Zagros Mountains, southwest
Iran: Facies, 57(3), 431- 446.
-SHABAFROOZ, R., MAHBOUBI, A., VAZIRI-MOGHADDAM, H., MOUSSAVI-HARAMI, R.,
GHABEISHAVI, A., and AL-AASM, I.S., 2015, Facies analysis and carbonate ramp evolution of Oligo-
Miocene Asmari Formation in the Gachsaran and Bibi-Hakimeh oilfiels and the nearby Mish anticline, Zagros
Basin, Iran: Neues Jahrbuch für Geologie und Paläontologie-Abhandlungen, 276(1), 121-146.
-SOLTANIAN, N., SEYRAFIAN A., and VAZIRI-MOGHADDAM, H., 2011, Biostratigraphy and paleo-
ecological implications in microfacies of the Asmari Formation (Oligocene), Naura anticline (Interior Fars of
the Zagros Basin), Iran: Carbonates Evaporites, 26(2), 167- 180.
-VAN BUCHEM, F.S.P., ALLAN, T.L., LAURSEN, G.V., LOTFPUR, M., MOALLEMI, A., MONIBI, S.,
MOTIEI, H., PICKARD, N.a.H., TAHMASBI, A.R., VEDRENE, V., and VINCENT, B., 2010, Regional
stratigraphic architecture and reservoir types of the Oligo-Miocene deposits in the Dezful Embayment (Asmari
and Pabdeh formations) SW Iran: 329, 219-263.
-VAZIRI-MOGHADDAM, H., SEYRAFIAN, A., TAHERI, A., and MOTIEI, H., 2010, Oligocene-Miocene
ramp system (Asmari Formation) in the NW of Zagros Basin, Iran: Microfacies, paleoenvironment and
depositional sequence: Revisita Mexicana de Ciencia Geologicals, 27, 56-71.
-WILSON, J.L., 1975, Carbonate facies in geologic history: Berlin, Heidelberg, New York. Springer, 471.
-WRIGHT, V.P., 1992, A revised classification of limestones, sedimentary: Geology, 76, 177-185.

17. Oligocene microfacies and sedimentary environment of
the Asmari Formation at northwest of Deris village, west
of Fars province: correlation with three other sections in
Zagros Basin
Received: November 2015, Accepted: Januvary 2016
Abstract
In this disquisition, Oligocene (Rupelian-Chattian) microfacies and sedimentary environment
of the Asmari Formation at the northwest of Deris village, located in interior Fars zone of the
Zagros Basin have been interpreted. The coordinates of such section are N: 29o 41' 59'', E:
51o 32' 26''. The Asmari Formation deposits in this section are divided into 5 lithological
units and consist of 460 m thin, medium, thick and massive bedded, gray and cream to gray
limestone, slightly dolomitic with nodular and marly interbedded. By study of hyaline benthic
foraminifera genera and non-foraminifera, and also recognition of some properties such as
skeletal ingredient associations and sedimentary textures of thin sections, 14 microfacies
have been introduced for the Asmari Formation. Gradual perpendicular changes of these
microfacies represent that settling the Asmari Formation deposits took place in a homoclinal
rapm. This homoclinal ramp consists of middle ramp and inner ramp, that are separated by
shoal environment. Middle ramp is recognized by presence and dominition hyaline benthic
foraminifera, coralline red algae and echinoids. The most significant skeletal debris of inner
ramp are porcelainous foraminifera. To compare the thickness, age and sedimentary
environment, zonal correlation of the Asmari Formation done in Deris section with three
other sections (Naura anticline, Dill anticline and Dehloran) in the Zagros Basin. This
correlation represent that the age of the Asmari Formation gets younger to the deeper parts
of the foreland basin of the Zagros.
Key words: Zagros Basin, Interior Fars, Asmari Formation, Oligocene, Microfacies, Homoclinal
ramp.