黔北—川东南志留系层序格架下的沉积体系演化特征及有利区带预测

朱志军

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黔北—川东南志留系层序格架下的沉积体系演化特征及有利区带预测

朱志军

文章导航 > 沉积学报 > 2010 > 28(2): 243-253

朱志军. 黔北—川东南志留系层序格架下的沉积体系演化特征及有利区带预测[J]. 沉积学报, 2010, 28(2): 243-253.

引用本文:

朱志军. 黔北—川东南志留系层序格架下的沉积体系演化特征及有利区带预测[J]. 沉积学报, 2010, 28(2): 243-253.

ZHU Zhijun. Depositional System Evolution Characteristics in the Framework of Sequences of Silurian and Prediction of Favorable Zones in the Northern GuizhouSoutheastern Sichuan[J]. Acta Sedimentologica Sinica, 2010, 28(2): 243-253.

Citation:

朱志军. 黔北—川东南志留系层序格架下的沉积体系演化特征及有利区带预测[J]. 沉积学报, 2010, 28(2): 243-253.

引用本文:

朱志军. 黔北—川东南志留系层序格架下的沉积体系演化特征及有利区带预测[J]. 沉积学报, 2010, 28(2): 243-253.

Citation:

黔北—川东南志留系层序格架下的沉积体系演化特征及有利区带预测

朱志军

油气藏地质及开发工程国家重点实验室(成都理工大学)成都610059

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通讯作者:
朱志军

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文章访问数: 2032
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Depositional System Evolution Characteristics in the Framework of Sequences of Silurian and Prediction of Favorable Zones in the Northern GuizhouSoutheastern Sichuan

ZHU Zhijun

State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation (Chengdu University of Technology) Chengdu 610059

More Information

Corresponding author: ZHU Zhijun

摘要

摘要: 黔北—川东南志留系受加里东运动抬升剥蚀仅残留中、下统地层，通过大量钻井及野外露头资料的沉积学研究，应用层序地层学方法，划分出8个三级层序，其中下志留统龙马溪组2个（SSQ1~SSQ2），石牛栏组或小河坝组2个（SSQ3~SSQ4），中下志留统韩家店组4个（SSQ5~SSQ8），识别出三角洲、陆棚、碳酸盐台地3类沉积体系，在等时地层格架中探讨了各沉积体系特征及其平面展布。通过层序地层划分对比及有利沉积相带研究，指出了两类有利储集层：一类为台地浅滩相和台地前缘斜坡相礁滩型生物灰岩、颗粒灰岩储层，主要发育于石牛栏期三级层序SSQ3和SSQ4的高位体系域，纵向上分布于石牛栏组中、上部，横向上分布于研究区南部叙永—习水—观音桥一带；另一类为浅水陆棚碎屑岩储层，主要发育于小河坝期三级层序SSQ4高水位体系域，横向上分布于南川—石柱—利川等地。
- 黔北—川东南志留系层序地层沉积体系高位体系域
Abstract: Because of uplifting by Caledonian movement，most of the Silurian had been denuded and only its middle and lower series remained in the Northern GuizhouSoutheastern Sichuan. On the basis of the comprehensive study cores and log wells and outcrops, 8 sequences and 2 system tracts were divided by use of sequence stratigraphic method, there are two sequences (SSQ1~SSQ2)in Longmaxi Formation of the Lower Silurian，one sequence (SSQ3~SSQ4) in Xiaoheba Formation, four sequences(SSQ5~SSQ8) in middlelower Silurian Hanjiadian Formation. 3 depositional systems of delta, coastal and shelf were developed to explore the characteristics of the depositional systems and their planar distribution in isochronous stratigraphic framework. One is reef flat biolithite and granule limestone developed in the platform shallow facies and platform foreslope facies, mainly in highstand systematic tract of the third sequence SSQ3 and SSQ4 in the Shiniulan Age. The vertical distribution is in the middle and upper of the Shiniulan formation, and horizontal distribution in XuyongXishuiGuanyinqiao in the southern of the study area. The other is shallow continental shelf clasolite reservoir, mainly developed in highstand systems tract of the third sequence SSQ4 in the Xiaoheba Age, laterally distributed in NanchuanShizhuLichuan and other places.
- Northern GuizhouSoutheastern Sichuan

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[1]	朱世发, 崔航, 陈嘉豪, 骆高俊, 王文禹, 杨祎, 施翌. 浅水三角洲沉积体系与储层岩石学特征 . 沉积学报, 2021, 39(1): 126-139. doi: 10.14027/j.issn.1000-0550.2020.115
[2]	刘永福, 赵建华, 范秋海, 林畅松, 叶茂林, 范倩倩, 张荣茜. 塔北隆起中部白垩系卡普沙良群层序地层格架及沉积体系研究 . 沉积学报, 2014, 32(6): 1113-1122.
[3]	. 松辽盆地东南缘层序地层与沉积体系配置及演化——以梨树断陷西北部营城组地层为例 . 沉积学报, 2013, 31(1): 67-76.
[4]	陈旭. 塔里木盆地台盆区三叠系三级层序界面和体系域界面的识别与应用 . 沉积学报, 2011, 29(5): 917-925.
[5]	冯有良. 徐家围子断陷下白垩统营城组四段层序地层与沉积体系发育特征 . 沉积学报, 2011, 29(5): 889-905.
[6]	朱志军. 川西前陆盆地侏罗纪层序地层格架、沉积体系配置及演化 . 沉积学报, 2010, 28(3): 451-461.
[7]	刘秋宏. 海拉尔盆地呼和湖凹陷南屯组层序地层与沉积体系分析 . 沉积学报, 2010, 28(2): 227-234.
[8]	曾凡平. 柯坪—巴楚露头区海相地层声波速度与沉积体系的关系 . 沉积学报, 2009, 27(2): 312-318.
[9]	纪友亮. 冀中坳陷古近系沉积层序特征及其沉积体系的演化 . 沉积学报, 2009, 27(1): 48-56.
[10]	纪友亮. 断陷盆地油气汇聚体系与层序地层格架之间的关系研究 . 沉积学报, 2008, 26(4): 617-623.
[11]	杨俊生. 苏丹Muglad盆地Fula坳陷白垩系Abu Gabra组层序地层及沉积体系 . 沉积学报, 2008, 26(6): 994-1004.
[12]	管红. 南堡凹陷东营组层序地层格架与沉积体系 . 沉积学报, 2008, 26(5): 730-736.
[13]	唐洪三. 合肥盆地白垩纪层序地层格架、沉积体系配置及演化 . 沉积学报, 2008, 26(6): 982-993.
[14]	黄传炎. 板桥凹陷断裂陡坡带沙一段层序样式和沉积体系特征及其成藏模式研究 . 沉积学报, 2007, 25(3): 386-391.
[15]	赵俊青, 纪友亮, 夏斌, 任拥军, 张善文. 近岸水下扇沉积体系高精度层序地层学研究 . 沉积学报, 2005, 23(3): 490-497.
[16]	赵俊青, 纪友亮, 夏斌, 张善文, 刘宝明. 扇三角洲沉积体系高精度层序地层学研究 . 沉积学报, 2004, 22(2): 302-309.
[17]	刘景彦, 陈志勇, 林畅松, 吴志轩. 东海丽水西次凹古新统明月峰组层序—体系域分析及沉积体系展布 . 沉积学报, 2004, 22(3): 380-386.
[18]	许淑梅, 翟世奎, 李三忠, 周立宏. 歧口凹陷滩海区下第三系层序地层分析及沉积体系研究 . 沉积学报, 2001, 19(3): 363-367.
[19]	贾进华, 刘焕杰, 郭英海. 鄂尔多斯盆地西缘晚石炭世沉积体系与高频层序旋回——以呼鲁斯太剖面例析 . 沉积学报, 1999, 17(3): 397-402.
[20]	郑荣才, 刘文均, 李祥辉, 王洪峰, 陈源仁. 龙门山平驿铺组沉积体系及旋回层序研究^① . 沉积学报, 1997, 15(3): 1-7.

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黔北—川东南志留系层序格架下的沉积体系演化特征及有利区带预测

朱志军

油气藏地质及开发工程国家重点实验室(成都理工大学)成都610059

通讯作者: 朱志军

收稿日期: 1900-01-01
修回日期: 1900-01-01
刊出日期: 2010-04-10

关键词:

黔北—川东南志留系层序地层沉积体系高位体系域

摘要: 黔北—川东南志留系受加里东运动抬升剥蚀仅残留中、下统地层，通过大量钻井及野外露头资料的沉积学研究，应用层序地层学方法，划分出8个三级层序，其中下志留统龙马溪组2个（SSQ1~SSQ2），石牛栏组或小河坝组2个（SSQ3~SSQ4），中下志留统韩家店组4个（SSQ5~SSQ8），识别出三角洲、陆棚、碳酸盐台地3类沉积体系，在等时地层格架中探讨了各沉积体系特征及其平面展布。通过层序地层划分对比及有利沉积相带研究，指出了两类有利储集层：一类为台地浅滩相和台地前缘斜坡相礁滩型生物灰岩、颗粒灰岩储层，主要发育于石牛栏期三级层序SSQ3和SSQ4的高位体系域，纵向上分布于石牛栏组中、上部，横向上分布于研究区南部叙永—习水—观音桥一带；另一类为浅水陆棚碎屑岩储层，主要发育于小河坝期三级层序SSQ4高水位体系域，横向上分布于南川—石柱—利川等地。

English Abstract

Depositional System Evolution Characteristics in the Framework of Sequences of Silurian and Prediction of Favorable Zones in the Northern GuizhouSoutheastern Sichuan

ZHU Zhijun

State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation (Chengdu University of Technology) Chengdu 610059

Corresponding author: ZHU Zhijun

Received Date: 1900-01-01
Rev Recd Date: 1900-01-01
Publish Date: 2010-04-10

Keywords:

Northern GuizhouSoutheastern Sichuan

Abstract: Because of uplifting by Caledonian movement，most of the Silurian had been denuded and only its middle and lower series remained in the Northern GuizhouSoutheastern Sichuan. On the basis of the comprehensive study cores and log wells and outcrops, 8 sequences and 2 system tracts were divided by use of sequence stratigraphic method, there are two sequences (SSQ1~SSQ2)in Longmaxi Formation of the Lower Silurian，one sequence (SSQ3~SSQ4) in Xiaoheba Formation, four sequences(SSQ5~SSQ8) in middlelower Silurian Hanjiadian Formation. 3 depositional systems of delta, coastal and shelf were developed to explore the characteristics of the depositional systems and their planar distribution in isochronous stratigraphic framework. One is reef flat biolithite and granule limestone developed in the platform shallow facies and platform foreslope facies, mainly in highstand systematic tract of the third sequence SSQ3 and SSQ4 in the Shiniulan Age. The vertical distribution is in the middle and upper of the Shiniulan formation, and horizontal distribution in XuyongXishuiGuanyinqiao in the southern of the study area. The other is shallow continental shelf clasolite reservoir, mainly developed in highstand systems tract of the third sequence SSQ4 in the Xiaoheba Age, laterally distributed in NanchuanShizhuLichuan and other places.

朱志军. 黔北—川东南志留系层序格架下的沉积体系演化特征及有利区带预测[J]. 沉积学报, 2010, 28(2): 243-253.

引用本文:

朱志军. 黔北—川东南志留系层序格架下的沉积体系演化特征及有利区带预测[J]. 沉积学报, 2010, 28(2): 243-253.

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黔北—川东南志留系层序格架下的沉积体系演化特征及有利区带预测

通讯作者:
朱志军

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Depositional System Evolution Characteristics in the Framework of Sequences of Silurian and Prediction of Favorable Zones in the Northern GuizhouSoutheastern Sichuan

Corresponding author: ZHU Zhijun

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黔北—川东南志留系层序格架下的沉积体系演化特征及有利区带预测

油气藏地质及开发工程国家重点实验室(成都理工大学)成都610059

通讯作者: 朱志军

English Abstract

Depositional System Evolution Characteristics in the Framework of Sequences of Silurian and Prediction of Favorable Zones in the Northern GuizhouSoutheastern Sichuan

State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation (Chengdu University of Technology) Chengdu 610059

Corresponding author: ZHU Zhijun

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黔北—川东南志留系层序格架下的沉积体系演化特征及有利区带预测

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Depositional System Evolution Characteristics in the Framework of Sequences of Silurian and Prediction of Favorable Zones in the Northern GuizhouSoutheastern Sichuan

Corresponding author: ZHU Zhijun

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黔北—川东南志留系层序格架下的沉积体系演化特征及有利区带预测

油气藏地质及开发工程国家重点实验室(成都理工大学)成都610059

通讯作者: 朱志军

English Abstract

Depositional System Evolution Characteristics in the Framework of Sequences of Silurian and Prediction of Favorable Zones in the Northern GuizhouSoutheastern Sichuan

State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation (Chengdu University of Technology) Chengdu 610059

Corresponding author: ZHU Zhijun

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