2010Lithologic ReservoirsRequires access

Differential tectonic movement of Yanchang Formation in southwestern margin of Ordos Basin and its geologic significance

Mingji Zhang

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Abstract

Huanxian-Zhenyuan area is one of the major exploration areas in southwestern margin of Ordos Basin in recent years.Some newgeology phenomenons appeared and were cared in the exploration.Based on the analysis of tuff,seismites and limestone gravel in Chang 7 to Chang 6 reservoir and thicken layers in Chang 7 to Chang 1 reservoir,it is believed that areal tectonic setting during Chang 7 to Chang 6 depositional stage is different from that during Chang 9 to Chang 8 depositional stage,which results in different formations,different sequence,different sedimentary settings,different lithologies and different reservoir properties.Different exploration methods are proposed for different layers and different reservoirs.

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What this paper is about

Huanxian-Zhenyuan area is one of the major exploration areas in southwestern margin of Ordos Basin in recent years.Some newgeology phenomenons appeared and were cared in the exploration.Based on the analysis of tuff,seismites and limestone gravel in Chang 7 to Chang 6 reservoir and thicken layers in Chang 7 to Chang 1 reservoir,it is believed that areal tectonic setting during Chang 7 to Chang 6 depositional stage is different from that during Chang 9 to Chang 8 depositional stage,which results in different formations,different sequence,different sedimentary settings,different lithologies and different reservoir properties.Different exploration methods are proposed for different layers and different reservoirs.

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Available abstract

Huanxian-Zhenyuan area is one of the major exploration areas in southwestern margin of Ordos Basin in recent years.Some newgeology phenomenons appeared and were cared in the exploration.Based on the analysis of tuff,seismites and limestone gravel in Chang 7 to Chang 6 reservoir and thicken layers in Chang 7 to Chang 1 reservoir,it is believed that areal tectonic setting during Chang 7 to Chang 6 depositional stage is different from that during Chang 9 to Chang 8 depositional stage,which results in different formations,different sequence,different sedimentary settings,different lithologies and different reservoir properties.Different exploration methods are proposed for different layers and different reservoirs.

Key concepts: Geology, Sedimentary depositional environment, Lithology, Structural basin, Tectonics, Sedimentary rock, Geomorphology, Geochemistry

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