Hydrothermal silicification and its impact on Lower–Middle Ordovician carbonates in Shunnan area, Tarim Basin, NW China

The Shunnan area is a newly discovered hydrocarbon field in Shuntuoguole lower uplift, in which the host rocks are Lower–Middle Ordovician carbonates. The carbonate reservoirs are well affected by hydrothermal silicification with well‐preserved intercrystalline pore of replacement quartz and megaqua...

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Veröffentlicht in:	Geological journal (Chichester, England) England), 2022-09, Vol.57 (9), p.3538-3557
Hauptverfasser:	Ye, Ning, Li, Yingtao, Huang, Baiwen, Xi, Binbin, Jiang, Hong, Lu, Ziye, Chen, Qianglu, You, Donghua, Xu, Jin
Format:	Artikel
Sprache:	eng
Schlagworte:	Calcite Carbonate rocks Carbonates Cementation Cements Chert Cherts Depth Diagenesis Evolution Fault detection Fractures Geological faults hydrothermal silicification Limestone Lithofacies Membrane permeability Mudstone Ordovician Permeability Petrography Petrology Pores Porosity Precursors Quartz reservoir quality Reservoirs secondary pore Silica Silicification Silicon dioxide Tarim Basin Temperature Uplift
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