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Metasomatism consists of volume-by-volume replacement of minerals androcks, as evidenced by pseudomorphs, preservation of older textures, and bulging contacts withwalls which do not «match». Serious petrographers admit that microscopic textures may often beexplained in different ways, and refer to geological and geochemical considerations for ...
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A HIMU‐Like Endmember Hiding in the Turkana Depression Continental Lithospheric Mantle
The fate of continental lithosphere during rifting is central to the process of continental extension. The continental lithospheric mantle comprises both depleted and enriched domains that may contribute to magma generation during extension.
Andrew R. Bollinger +3 more
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Ankara’nın yaklaşık 50-60 km güneybatısında yer alan erken Miyosen yaşlı Oyaca, Kedikayası ve Boyalık dasitleri adakit ve/veya adakitik kayaçlara benzer özelliklere sahiptir.
Pınar ŞEN, Erdal ŞEN
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Base oil and gas complex, of which the new area exploration in the Eastern region of Ukraine consists of lower (subsurface section Precambrian basement) and upper (Precambrian weathering crust, roofing layers of sedimentary rock) sub.
V. P. Lebed
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Petrological and geochemical features of Biga Peninsula granitoids, NW Anatolia, Turkey
Ümit AYDIN +3 more
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Why metasomatic fronts are really metasomatic sides
Geology, 1995Back-scattered electron microscope images of metasomatic calc-silicate rocks demonstrate complex mineral growth patterns; often oscillatory zoning defines a euhedral or subhedral morphology. We infer from this the existence of an appreciable transient porosity (up to a few percent) during metasomatic calc-silicate growth, and argue that porous ...
Bruce W. D. Yardley, Geoff E. Lloyd
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