Favorable reservoir facies tracts in the Changxing-Feixianguan formations of Sichuan Basin
Zhu Qiuying
Abstract
Zhu Qiuying
Abstract
In order to predict and optimize favorable exploration plays,we used the theory and methodology of sequence stratigraphy to divide the Changxing-Feixianguan formations in the Sichuan Basin into 8 sequences and 17 system tracts and to establish a relevant sequence stratigraphic framework.A study on the distribution of depositional facies within the sequence stratigraphic framework revealed that favorable platform-margin reef flat reservoir facies tract occurs in the Changxing-Feixianguan formations.This facies tract is controlled by Kaijiang-Liangping,Exi-Chengkou and Chuanxi(West Sichuan Basin)troughs and is in banded distribution on both sides of the troughs.Based on the prediction results of the platform-margin reef flat facies and in combination with various geologic data,we identified 3 types and 8 subtypes of favorable reservoir facies tracts.Type-Ⅰ is platform-margin reef flat facies which is distributed on the western side of Exi-Chengkou trough,both eastern and western sides of Kaijiang-Liangping trough,and both sides of Chuanxi trough.Type-Ⅱ is inner-platform reef flat facies which is distributed in Chuanxi and Chuanzhong(Central Sichuan Basin)areas.Type-III is inner-platform dolomite which is distributed in Chuannan(South Sichuan Basin)and Chuandong(East Sichuan Basin)areas.Among them,type-Ⅰ facies tract is the most favorable for exploration and the focus of current exploration,while as a supplement to type-I,the exploration of type-Ⅱ facies tract should be further strengthened though certain breakthrough has been made now.In contrast,type-III facies tract is large in area but low in exploration maturity as a whole,so comprehensive geologic study should be enhanced.
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In order to predict and optimize favorable exploration plays,we used the theory and methodology of sequence stratigraphy to divide the Changxing-Feixianguan formations in the Sichuan Basin into 8 sequences and 17 system tracts and to establish a relevant sequence stratigraphic framework.A study on the distribution of depositional facies within the sequence stratigraphic framework revealed that favorable platform-margin reef flat reservoir facies tract occurs in the Changxing-Feixianguan formations.This facies tract is controlled by Kaijiang-Liangping,Exi-Chengkou and Chuanxi(West Sichuan Basin)troughs and is in banded distribution on both sides of the troughs.Based on the prediction results of the platform-margin reef flat facies and in combination with various geologic data,we identified 3 types and 8 subtypes of favorable reservoir facies tracts.Type-Ⅰ is platform-margin reef flat facies which is distributed on the western side of Exi-Chengkou trough,both eastern and western sides of Kaijiang-Liangping trough,and both sides of Chuanxi trough.Type-Ⅱ is inner-platform reef flat facies which is distributed in Chuanxi and Chuanzhong(Central Sichuan Basin)areas.Type-III is inner-platform dolomite which is distributed in Chuannan(South Sichuan Basin)and Chuandong(East Sichuan Basin)areas.Among them,type-Ⅰ facies tract is the most favorable for exploration and the focus of current exploration,while as a supplement to type-I,the exploration of type-Ⅱ facies tract should be further strengthened though certain breakthrough has been made now.In contrast,type-III facies tract is large in area but low in exploration maturity as a whole,so comprehensive geologic study should be enhanced.
Key concepts: Facies, Geology, Trough (economics), Structural basin, Reef, Sequence stratigraphy, Sichuan basin, Paleontology