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Ophiolite ppt
Ophiolite ppt
Ajoy Raj Saikia
The name ophiolite derived from Greek root which means Ophio : snake or serpent Litho : Stone The green colour, structure and texture of sheared ultramafic rocks is similar to some serpents Economically : Massive Sulphide It founded within pillow lava most of massive Sulphide associated in ophiolites have well developed Gossans (bright colored iron oxide, hydroxides, and sulfides) which is very rich in gold. Chromite Stratiform (be tabular or pencil shape) or podiform (irregular shape) within ultra-mafic rocks These deposits are developed on serpentinite peridotite Laterites (nickel and iron) Asbestos Talc Magenesite ophiolite sequence : Sediments Pillow Lavas Dykes Gabbros Layered Gabbro Layered Peridotite Upper mantle
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Continental rifts are regions of extensional deformation where the entire thickness of the lithosphere has deformed under the influence of deviatoric tension. Rifts represent the initial stage of continental break-up where extension may lead to lithospheric rupture and the formation of a new ocean basin.
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Ophiolite ppt
Ophiolite ppt
Ajoy Raj Saikia
The name ophiolite derived from Greek root which means Ophio : snake or serpent Litho : Stone The green colour, structure and texture of sheared ultramafic rocks is similar to some serpents Economically : Massive Sulphide It founded within pillow lava most of massive Sulphide associated in ophiolites have well developed Gossans (bright colored iron oxide, hydroxides, and sulfides) which is very rich in gold. Chromite Stratiform (be tabular or pencil shape) or podiform (irregular shape) within ultra-mafic rocks These deposits are developed on serpentinite peridotite Laterites (nickel and iron) Asbestos Talc Magenesite ophiolite sequence : Sediments Pillow Lavas Dykes Gabbros Layered Gabbro Layered Peridotite Upper mantle
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Anorthosite
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Continental rifts are regions of extensional deformation where the entire thickness of the lithosphere has deformed under the influence of deviatoric tension. Rifts represent the initial stage of continental break-up where extension may lead to lithospheric rupture and the formation of a new ocean basin.
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Komattite Named after the Komati River in South Africa. first described by Morris and Richard (twins) for ultramafic units in the Barberton Greenstone belt of South Africa. Mostly of komatiite are Archean age distributed in the Archaean shield areas. Also a few are Proterozoic and Phanerozoic. In all ages komatiites are highly magnesium. Mostly a volcanic rock; occasionally intrusive. Mafic rocks were identified as extrusive because of their volcanic textures and structures, and they seem to have been accepted as a normal component of Archean volcanic successions, Abitibi in Canada. The ultramafic rocks were interpreted as intrusive which are founded as sills and dykes, Barberton in South Africa. Spinifex texture-typical of Komatiites:
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The name ophiolite derived from Greek root which means Ophio : snake or serpent Litho : Stone The green colour, structure and texture of sheared ultramafic rocks is similar to some serpents The term ophiolite was initially given to dark green shiny outcrops which composed of serpentines (serpentinite rocks) later on become used not only to a single rock , but also to an association of related rock types which are found as a consistent of upper mantle rocks and oceanic crust. ophiolite sequence Sediments Pillow Lavas Dykes Gabbros Layered Gabbro Layered Peridotite Upper mantle
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Komattite Named after the Komati River in South Africa. first described by Morris and Richard (twins) for ultramafic units in the Barberton Greenstone belt of South Africa. Mostly of komatiite are Archean age distributed in the Archaean shield areas. Also a few are Proterozoic and Phanerozoic. In all ages komatiites are highly magnesium. Mostly a volcanic rock; occasionally intrusive. Mafic rocks were identified as extrusive because of their volcanic textures and structures, and they seem to have been accepted as a normal component of Archean volcanic successions, Abitibi in Canada. The ultramafic rocks were interpreted as intrusive which are founded as sills and dykes, Barberton in South Africa. Spinifex texture-typical of Komatiites:
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The name ophiolite derived from Greek root which means Ophio : snake or serpent Litho : Stone The green colour, structure and texture of sheared ultramafic rocks is similar to some serpents The term ophiolite was initially given to dark green shiny outcrops which composed of serpentines (serpentinite rocks) later on become used not only to a single rock , but also to an association of related rock types which are found as a consistent of upper mantle rocks and oceanic crust. ophiolite sequence Sediments Pillow Lavas Dykes Gabbros Layered Gabbro Layered Peridotite Upper mantle
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