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BASIC
GEOLOGY
4.
PETROGRAPHY
The rock cycle - stages, places and processes
Magma
• silicate-rich melt
• originates from the partial melt of the lower crust and the upper
mantel (50-200 km bs)
• Principal elements are O, Si, Al, Ca, Na, K, Fe and Mg
Extrusive – Intrusive
Calc-alkaline – Alkaline – Tholeiitic
Basic – Intermediate - Acidic
IGNEOUS ROCKS
Bowen’s reaction series
Anorthite 1:4
Albite 3:8
Streckeisen’s classification of igneous rocks
Total Alkali Silica (TAS) diagram
Ultramafic rocks (peridotites) – mafic mineral constituents
(olivine, pyroxene, hornblende)
Gabbros – composed Ca-rich plagioclase feldspar as well as
pyroxene, olivine, hornblende)
Diorites – Ca-Na-bearing plagioclase feldspar with
hornblende, biotite and pyroxene
Syenites – intermediate plutonic rocks with alkali feldspars and mafic
constituents (biotite and hornblende)
Basalts – volcanic equivalents of
gabbros
Andesites – volcanic equivalents of
diorite
Trachytes – volcanic equivalent
od syenites
Rhyolites – volcanic equivalents of granitic rocks
Granitic rocks - composed of quartz, plagioclase and orthoclase,
micas and amphibole
Classification and nomenclature of pyroclastics rocks
SEDIMENTARY ROCKS
• weathering of pre-existing rocks
• transportation of the material away from the original site
• deposition of the eroded material
1. Clastic rocks
consisting rock and mineral fragments
2. Chemical rocks
consisting chemical precipitates
3. Organic rocks
consisting organic material
Ternary diagrams for classification of siliciclastic rocks
CLASTIC ROCKS: Conglomerates – consolidated
deposits of gravel
CLASTIC ROCKS: Sandstones
CLASTIC ROCKS: Silstones
CLASTIC ROCKS: Mudstone
CHEMICAL ROCKS: Limestones
CHEMICAL ROCKS: Evaporites
Rock salt Gypsum
Distribution of salt concentration and evaporation in a lagoon
Levels of coalification according to the
change of gas content „vitrinite reflection”
CHEMICAL ROCKS: Coals
Some types of oil traps
METAMORPHIC ROCKS
Changes in temperature and pressure
Changes in chemistry of pore fliuds
New minerals, new texture and new structure
Contact metamorphism
local phenomenon associated with thermal (and chemical) changes near
the contacts of igneous intrusions
Regional metamorphism
Develops in the roots of mountain belt along convergent plate boundaries
Main forms of contact metamorphism
Subdivision of regional
metamorphism according
to the degree of
metamorphism and the
original (parent) rock
Slates
Low grade metamorphism, excellent foliation (slaty cleavage)
Schists
Medium-grade metamorphism, excellent foliation (schistosity) as a result
of parallel arrangement of platy minerals
Gneiss
High-grade metamorphism, coarse-grained, alternating layering of
dark and light minerals
Non-foliated metamorphic rocks
Marble Quartzite
Amphibolite
THANK YOU FOR YOUR ATTENTION!

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Basic Geology and Geomorphology power point