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QIAO Zhanfeng. Characteristics and Evolution Model of Sequence Stratigraphy of Feixianguan Formation in the Northeast of Sichuan Basin[J]. Acta Sedimentologica Sinica, 2010, 28(3): 462-470.
Citation: QIAO Zhanfeng. Characteristics and Evolution Model of Sequence Stratigraphy of Feixianguan Formation in the Northeast of Sichuan Basin[J]. Acta Sedimentologica Sinica, 2010, 28(3): 462-470.

Characteristics and Evolution Model of Sequence Stratigraphy of Feixianguan Formation in the Northeast of Sichuan Basin

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  • Corresponding author: QIAO Zhanfeng
  • Received Date: 1900-01-01
  • Rev Recd Date: 1900-01-01
  • Publish Date: 2010-06-10
  • Based on the knowledge of the sedimentary and tectonic settings in the northeast of the Sichuan basin, using the different methods, such as: outcrop, core, welllogging and seismic, and so on, with the careful analysis of the sequence surfaces, facies section, the stacking pattern, welllogging curves and seismic sequence stratigraphy, and so on, there are 2 thirdorder sequences distinguished in the Feixianguan Formation in the northeast of the Sichuan basin, both of which include the LST, TST and HST. Furthermore, using the theory of the sequence stratigraphy, by establishing the framework of the sequence stratigraphy of the Feixianguan Formation in the northeast of the Sichuan basin, based on the analysis of the control factors of the sequence stratigraphy, the evolution model of the sequence stratigraphy of the Feixianguan Formation is established in the northeast of the Sichuan basin. Furthermore, the distribution of the shoal is discussed in the framework of the sequence evolution; it is important to the further exploration of the hydrocarbon in the northeast of the Sichuan basin. 
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    Created with Highcharts 5.0.7Chart context menuAccess Area Distribution其他: 2.5 %其他: 2.5 %其他: 1.4 %其他: 1.4 %China: 0.4 %China: 0.4 %United States: 1.1 %United States: 1.1 %上海: 0.4 %上海: 0.4 %中卫: 0.7 %中卫: 0.7 %乌鲁木齐: 0.4 %乌鲁木齐: 0.4 %乐山: 0.4 %乐山: 0.4 %兰州: 0.4 %兰州: 0.4 %凉山: 0.4 %凉山: 0.4 %北京: 13.1 %北京: 13.1 %南京: 0.4 %南京: 0.4 %南充: 0.4 %南充: 0.4 %台州: 0.7 %台州: 0.7 %哥伦布: 0.4 %哥伦布: 0.4 %城南: 0.4 %城南: 0.4 %大庆: 0.4 %大庆: 0.4 %天津: 1.1 %天津: 1.1 %宝鸡: 0.7 %宝鸡: 0.7 %宣城: 0.4 %宣城: 0.4 %常州: 0.4 %常州: 0.4 %广州: 0.7 %广州: 0.7 %库比蒂诺: 0.4 %库比蒂诺: 0.4 %张家口: 3.5 %张家口: 3.5 %成都: 2.8 %成都: 2.8 %扬州: 0.4 %扬州: 0.4 %杭州: 2.1 %杭州: 2.1 %武汉: 2.8 %武汉: 2.8 %沈阳: 0.4 %沈阳: 0.4 %泉州: 0.4 %泉州: 0.4 %泰安: 0.4 %泰安: 0.4 %济南: 1.1 %济南: 1.1 %深圳: 0.4 %深圳: 0.4 %湖州: 1.8 %湖州: 1.8 %湛江: 0.4 %湛江: 0.4 %漯河: 1.4 %漯河: 1.4 %牡丹江: 0.4 %牡丹江: 0.4 %石家庄: 0.4 %石家庄: 0.4 %芒廷维尤: 12.4 %芒廷维尤: 12.4 %芝加哥: 2.5 %芝加哥: 2.5 %苏州: 0.7 %苏州: 0.7 %荆州: 0.4 %荆州: 0.4 %衡阳: 0.4 %衡阳: 0.4 %衢州: 1.8 %衢州: 1.8 %西宁: 31.9 %西宁: 31.9 %西安: 0.4 %西安: 0.4 %贵阳: 0.4 %贵阳: 0.4 %达州: 0.4 %达州: 0.4 %通辽: 0.4 %通辽: 0.4 %遂宁: 0.4 %遂宁: 0.4 %郑州: 0.4 %郑州: 0.4 %重庆: 1.1 %重庆: 1.1 %金昌: 0.4 %金昌: 0.4 %长沙: 0.7 %长沙: 0.7 %黄冈: 0.4 %黄冈: 0.4 %其他其他ChinaUnited States上海中卫乌鲁木齐乐山兰州凉山北京南京南充台州哥伦布城南大庆天津宝鸡宣城常州广州库比蒂诺张家口成都扬州杭州武汉沈阳泉州泰安济南深圳湖州湛江漯河牡丹江石家庄芒廷维尤芝加哥苏州荆州衡阳衢州西宁西安贵阳达州通辽遂宁郑州重庆金昌长沙黄冈
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  • Received:  1900-01-01
  • Revised:  1900-01-01
  • Published:  2010-06-10

Characteristics and Evolution Model of Sequence Stratigraphy of Feixianguan Formation in the Northeast of Sichuan Basin

    Corresponding author: QIAO Zhanfeng

Abstract: Based on the knowledge of the sedimentary and tectonic settings in the northeast of the Sichuan basin, using the different methods, such as: outcrop, core, welllogging and seismic, and so on, with the careful analysis of the sequence surfaces, facies section, the stacking pattern, welllogging curves and seismic sequence stratigraphy, and so on, there are 2 thirdorder sequences distinguished in the Feixianguan Formation in the northeast of the Sichuan basin, both of which include the LST, TST and HST. Furthermore, using the theory of the sequence stratigraphy, by establishing the framework of the sequence stratigraphy of the Feixianguan Formation in the northeast of the Sichuan basin, based on the analysis of the control factors of the sequence stratigraphy, the evolution model of the sequence stratigraphy of the Feixianguan Formation is established in the northeast of the Sichuan basin. Furthermore, the distribution of the shoal is discussed in the framework of the sequence evolution; it is important to the further exploration of the hydrocarbon in the northeast of the Sichuan basin. 

QIAO Zhanfeng. Characteristics and Evolution Model of Sequence Stratigraphy of Feixianguan Formation in the Northeast of Sichuan Basin[J]. Acta Sedimentologica Sinica, 2010, 28(3): 462-470.
Citation: QIAO Zhanfeng. Characteristics and Evolution Model of Sequence Stratigraphy of Feixianguan Formation in the Northeast of Sichuan Basin[J]. Acta Sedimentologica Sinica, 2010, 28(3): 462-470.

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