Multiple dolomitization and later hydrothermal alteration on the Upper Cambrian-Lower Ordovician carbonates in the northern Tarim Basin, China

Thick Upper Cambrian-Lower Ordovician carbonates were deposited on a shallow marine platform in the northern Tarim Basin, which were extensively dolomitized, particularly for the Upper Cambrian carbonates. The resulting dolomite rocks are predominantly composed of matrix dolomites with minor cement...

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Veröffentlicht in:	Marine and petroleum geology 2016-04, Vol.72, p.295-316
Hauptverfasser:	Guo, Chuan, Chen, Daizhao, Qing, Hairuo, Dong, Shaofeng, Li, Guorong, Wang, Dan, Qian, Yixiong, Liu, Cunge
Format:	Artikel
Sprache:	eng
Schlagworte:	Basins Burial dolomitization Carbonates Cements Crystal structure Dolomite Fluid dynamics Fluid flow Fluids Hydrothermal alteration Marine Reflux dolomitization Tarim basin Upper Cambrian-lower Ordovician
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