中新生代天山隆升及其南北盆地分异与沉积环境演化

高志勇; 周川闽; 冯佳睿; 吴昊; 李雯

doi:10.14027/j.cnki.cjxb.2016.03.001

ISSN 1000-0550 CN 62-1038/P

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中新生代天山隆升及其南北盆地分异与沉积环境演化

高志勇, 周川闽, 冯佳睿, 吴昊, 李雯

文章导航 > 沉积学报 > 2016 > 34(3): 415-435

高志勇, 周川闽, 冯佳睿, 吴昊, 李雯. 中新生代天山隆升及其南北盆地分异与沉积环境演化[J]. 沉积学报, 2016, 34(3): 415-435. doi: 10.14027/j.cnki.cjxb.2016.03.001

引用本文:

高志勇, 周川闽, 冯佳睿, 吴昊, 李雯. 中新生代天山隆升及其南北盆地分异与沉积环境演化[J]. 沉积学报, 2016, 34(3): 415-435. doi: 10.14027/j.cnki.cjxb.2016.03.001

GAO ZhiYong, ZHOU ChuanMin, FENG JiaRui, WU Hao, LI Wen. Relationship between the Tianshan Mountains Uplift and Depositional Environment Evolution of the Basins in Mesozoic-Cenozoic[J]. Acta Sedimentologica Sinica, 2016, 34(3): 415-435. doi: 10.14027/j.cnki.cjxb.2016.03.001

Citation:

GAO ZhiYong, ZHOU ChuanMin, FENG JiaRui, WU Hao, LI Wen. Relationship between the Tianshan Mountains Uplift and Depositional Environment Evolution of the Basins in Mesozoic-Cenozoic[J]. Acta Sedimentologica Sinica, 2016, 34(3): 415-435. doi: 10.14027/j.cnki.cjxb.2016.03.001

高志勇, 周川闽, 冯佳睿, 吴昊, 李雯. 中新生代天山隆升及其南北盆地分异与沉积环境演化[J]. 沉积学报, 2016, 34(3): 415-435. doi: 10.14027/j.cnki.cjxb.2016.03.001

引用本文:

高志勇, 周川闽, 冯佳睿, 吴昊, 李雯. 中新生代天山隆升及其南北盆地分异与沉积环境演化[J]. 沉积学报, 2016, 34(3): 415-435. doi: 10.14027/j.cnki.cjxb.2016.03.001

Citation:

GAO ZhiYong, ZHOU ChuanMin, FENG JiaRui, WU Hao, LI Wen. Relationship between the Tianshan Mountains Uplift and Depositional Environment Evolution of the Basins in Mesozoic-Cenozoic[J]. Acta Sedimentologica Sinica, 2016, 34(3): 415-435. doi: 10.14027/j.cnki.cjxb.2016.03.001

中新生代天山隆升及其南北盆地分异与沉积环境演化

doi: 10.14027/j.cnki.cjxb.2016.03.001

1.
中国石油勘探开发研究院实验研究中心北京 100083;
2.
提高石油采收率国家重点实验室(中国石油勘探开发研究院) 北京 100083;
3.
中国地震局北京 100036;
4.
中国地质大学地球科学与资源学院北京 100083

基金项目: 国家科技重大专项课题(2011ZX05003-002,2016ZX05003-001);中国石油股份公司科技项目(2014B-0408)

详细信息

作者简介:
高志勇,男,1974年出生,高级工程师,沉积学及油气储层地质,E-mail:gzybox@163.com

中图分类号: P548;P618.13

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文章访问数: 617
HTML全文浏览量: 37
PDF下载量: 736
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Relationship between the Tianshan Mountains Uplift and Depositional Environment Evolution of the Basins in Mesozoic-Cenozoic

1.
Petroleum Geology Research and Laboratory Center, RIPED, Beijing 100083, China;
2.
State Key Laboratory of Enhanced Oil Recovery (Research Institute of Petroleum Exploration and Development), Beijing 100083, China;
3.
China Earthquake Administration, Beijing 100036, China;
4.
China University of Geosciences, Beijing, 100083, China

Funds: National Science and Technology Major Project，No.2011ZX05003-002, 2016ZX05003-001; PetroChina Science and Technology Project, No.2014B-0408

摘要

摘要: 明确中生代以来天山隆升的时间顺序、隆升范围,及其与南北两侧盆地的沉积环境演化之间的关系,是天山两侧准噶尔盆地、吐哈盆地与塔里木等盆地原型恢复研究的重要需求。通过分析天山南北主要盆地类型、沉积充填、古气候变化,物源属性、边缘相带迁移反映的物源区远近变化与古水流特征,以及大量磷灰石裂变径迹测年数据认为,中新生代天山主要存在晚三叠世—早侏罗世、晚侏罗世—早白垩世、晚白垩世—始新世、中新世—第四纪的四期阶段隆升。在此基础上,编制了早侏罗世早期—第四纪的天山隆升范围及其南北盆地的沉积环境演化图,表明天山的四阶段隆升控制了北疆与南疆盆地由早、中侏罗世统一泛湖盆至晚侏罗—早白垩世盆地开始分异,再到新近纪以来彻底分割成独立盆地的沉积演化过程。同时,明确了天山南北两侧各盆地储层、烃源岩及盖层的重要形成期与天山隆升的关系,对有效拓展油气勘探范围有所启示。
- 天山隆升 /
- 中新生代 /
- 新疆地区 /
- 沉积环境 /
- 储层与烃源岩
Abstract: Clearing the relationship among since Mesozoic Tianshan uplift of time sequence, scope, and north and south on both sides of the basin sedimentary evolution, which shows on both sides of Tianshan mountain, Tuha Basin in Junggar Basin and Tarim Basin has important demand to recovery basin protoeype. Through the analysis of a large number of previous apatite fission track dating data, quantitative calculation of gravel transport distance and provenance, the nature of the basin, depositional filling and palaeoclimate changing and the ancient flow, it is believed that of there are four periods of stage uplift of Miocene to Quaternary. They are Late Triassic to Early Jurassic, Late Jurassic - Early Cretaceous and Late Cretaceous to Eocene. The uplift range are two small and two large ones. On the analysis of the Tianshan mountains north and south on both sides of the basin on the basis of lithologic, stratigraphic and sedimentary characteristics, combination of Tianshan uplift mountain range and time, compiled the Early Jurassic to the early - to the south of Tianshan uplift area and its quaternary sedimentary facies evolution, it is considered that Tianshan uplift controlled the four phases of the unified by the early and Middle Jurassic in northern and southern Xinjiang Basin flood lake basin to the Late Jurassic and Early Cretaceous basin began to differentiation, to thoroughly split into independent sedimentary evolution of the basin since Neogene. At the same time, it is clear about the Tianshan mountains between the north and the south on both sides of the basin, hydrocarbon source rocks, reservoir and cap rock important formation to the Tianshan uplift. The understanding of clear and distribution of hydrocarbon source rock, reservoir rock development period is of great significance, also some enlightenment to effectively expanding the scope of oil and gas exploration.
- Tianshan mountains uplift /
- Mesozoic-Cenozoic /
- Xinjiang area /
- depositional environment /
- reservoir and hydrocarbon source rock

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[1]	庄其天, 何宏林, 魏荣珠, 王忠梅, 石峰, 闫纪元. 山西地堑系太原盆地晚新生代沉积环境演化及物源分析 . 沉积学报, 2024, 42(2): 486-501. doi: 10.14027/j.issn.1000-0550.2022.064
[2]	刘棠煊, 陈雷, 白森, 张金武, 乔崇, 程辉, 谭秀成, 秦何星. 沉积环境对页岩储层弹性特征的影响——以川南自贡地区龙马溪组页岩为例 . 沉积学报, 2023, (): -. doi: 10.14027/j.issn.1000-0550.2023.087
[3]	刘振, 马志鑫, 刘伟, 凌云. 重庆秀山小茶园地区南华纪大塘坡组沉积环境与锰矿产出规律 . 沉积学报, 2021, 39(3): 515-524. doi: 10.14027/j.issn.1000-0550.2020.109
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[5]	陈淑慧, 侯元立, 邵磊, 黄奇瑜, 乔培军, 崔宇驰, 孟宪博. 台湾始新统—中新统沉积物源与沉积环境 . 沉积学报, 2020, 38(2): 319-330. doi: 10.14027/j.issn.1000-0550.2019.037
[6]	宋慧波, 王芳, 胡斌. 晋中南地区上石炭统-下二叠统太原组碳酸盐岩中遗迹组构及其沉积环境 . 沉积学报, 2015, 33(6): 1126-1139. doi: 10.14027/j.cnki.cjxb.2015.06.006
[7]	时文革, 巩恩普, 褚亦功, 张永利, 姚玉增, 王铁晖, 马伟, 赵纯福. 新疆拜城新近系含铜岩系沉积体系及沉积环境 . 沉积学报, 2015, 33(6): 1074-1086. doi: 10.14027/j.cnki.cjxb.2015.06.002
[8]	李运振. 中国近海新生代盆地沉积环境演变分析 . 沉积学报, 2010, 28(6): 1066-1075.
[9]	田云涛. 桂西南柳桥地区上二叠统大隆组层状硅质岩成因和沉积环境 . 沉积学报, 2007, 25(5): 671-677.
[10]	胡瑛. 黄骅坳陷滩海三马地区烃源岩分子标志物特征及其沉积相指示意义 . 沉积学报, 2006, 24(3): 419-425.
[11]	陈戴生. 我国中、新生代盆地砂岩型铀矿沉积环境研究概述① . 沉积学报, 2006, 24(2): 223-228.
[12]	刘志飞, 王成善, 金玮, 伊海生, 郑洪波, 赵西西, 李亚林. 青藏高原沱沱河盆地渐新—中新世沉积环境分析 . 沉积学报, 2005, 23(2): 210-217.
[13]	柳永清, 高林志, 刘燕学. 苏皖辽地区新元古代微亮晶构造碳酸盐岩的沉积岩相与环境约束 . 沉积学报, 2005, 23(1): 49-59.
[14]	李忠, 王清晨, 王道轩, 林伟. 晚新生代天山隆升与库车坳陷构造转换的沉积约束 . 沉积学报, 2003, 21(1): 38-45.
[15]	刘秉理, 朱忠德, 肖传桃, 胡明毅. 鄂西地区早奥陶世分乡期生物群落演化与沉积环境变迁 . 沉积学报, 1997, 15(4): 97-102.
[16]	王东安, 陈瑞君. 新疆克兹扬鲁克一带泥盆系沉积岩特征及其沉积环境 . 沉积学报, 1995, 13(3): 13-22.
[17]	王国纯, 朱伟林. 东海盆地新生代沉积环境 . 沉积学报, 1992, 10(2): 100-108.
[18]	朱莲芳, 马宝林. 塔里木盆地阿克苏—柯坪地区寒武系—奥陶系的沉积环境 . 沉积学报, 1991, 9(2): 55-62.
[19]	史基安, 马宝林, 师育新. 新疆巴楚-柯坪地区上石炭统碳酸盐岩的沉积环境与成岩作用 . 沉积学报, 1990, 8(4): 59-67.
[20]	李书舜, 刘大成. 四川地区晚二叠世沉积环境与生物礁 . 沉积学报, 1988, 6(3): 112-117.

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中新生代天山隆升及其南北盆地分异与沉积环境演化

doi: 10.14027/j.cnki.cjxb.2016.03.001

1. 中国石油勘探开发研究院实验研究中心北京 100083;

2. 提高石油采收率国家重点实验室(中国石油勘探开发研究院) 北京 100083;

3. 中国地震局北京 100036;

4. 中国地质大学地球科学与资源学院北京 100083

基金项目: 国家科技重大专项课题(2011ZX05003-002,2016ZX05003-001);中国石油股份公司科技项目(2014B-0408)

作者简介:
高志勇,男,1974年出生,高级工程师,沉积学及油气储层地质,E-mail:gzybox@163.com

收稿日期: 2015-07-29
修回日期: 2015-11-12
刊出日期: 2016-06-10

中图分类号: P548;P618.13

关键词:

摘要: 明确中生代以来天山隆升的时间顺序、隆升范围,及其与南北两侧盆地的沉积环境演化之间的关系,是天山两侧准噶尔盆地、吐哈盆地与塔里木等盆地原型恢复研究的重要需求。通过分析天山南北主要盆地类型、沉积充填、古气候变化,物源属性、边缘相带迁移反映的物源区远近变化与古水流特征,以及大量磷灰石裂变径迹测年数据认为,中新生代天山主要存在晚三叠世—早侏罗世、晚侏罗世—早白垩世、晚白垩世—始新世、中新世—第四纪的四期阶段隆升。在此基础上,编制了早侏罗世早期—第四纪的天山隆升范围及其南北盆地的沉积环境演化图,表明天山的四阶段隆升控制了北疆与南疆盆地由早、中侏罗世统一泛湖盆至晚侏罗—早白垩世盆地开始分异,再到新近纪以来彻底分割成独立盆地的沉积演化过程。同时,明确了天山南北两侧各盆地储层、烃源岩及盖层的重要形成期与天山隆升的关系,对有效拓展油气勘探范围有所启示。

English Abstract

Relationship between the Tianshan Mountains Uplift and Depositional Environment Evolution of the Basins in Mesozoic-Cenozoic

1. Petroleum Geology Research and Laboratory Center, RIPED, Beijing 100083, China;

2. State Key Laboratory of Enhanced Oil Recovery (Research Institute of Petroleum Exploration and Development), Beijing 100083, China;

3. China Earthquake Administration, Beijing 100036, China;

4. China University of Geosciences, Beijing, 100083, China

Funds: National Science and Technology Major Project，No.2011ZX05003-002, 2016ZX05003-001; PetroChina Science and Technology Project, No.2014B-0408

Received Date: 2015-07-29
Rev Recd Date: 2015-11-12
Publish Date: 2016-06-10

Keywords:

Abstract: Clearing the relationship among since Mesozoic Tianshan uplift of time sequence, scope, and north and south on both sides of the basin sedimentary evolution, which shows on both sides of Tianshan mountain, Tuha Basin in Junggar Basin and Tarim Basin has important demand to recovery basin protoeype. Through the analysis of a large number of previous apatite fission track dating data, quantitative calculation of gravel transport distance and provenance, the nature of the basin, depositional filling and palaeoclimate changing and the ancient flow, it is believed that of there are four periods of stage uplift of Miocene to Quaternary. They are Late Triassic to Early Jurassic, Late Jurassic - Early Cretaceous and Late Cretaceous to Eocene. The uplift range are two small and two large ones. On the analysis of the Tianshan mountains north and south on both sides of the basin on the basis of lithologic, stratigraphic and sedimentary characteristics, combination of Tianshan uplift mountain range and time, compiled the Early Jurassic to the early - to the south of Tianshan uplift area and its quaternary sedimentary facies evolution, it is considered that Tianshan uplift controlled the four phases of the unified by the early and Middle Jurassic in northern and southern Xinjiang Basin flood lake basin to the Late Jurassic and Early Cretaceous basin began to differentiation, to thoroughly split into independent sedimentary evolution of the basin since Neogene. At the same time, it is clear about the Tianshan mountains between the north and the south on both sides of the basin, hydrocarbon source rocks, reservoir and cap rock important formation to the Tianshan uplift. The understanding of clear and distribution of hydrocarbon source rock, reservoir rock development period is of great significance, also some enlightenment to effectively expanding the scope of oil and gas exploration.

高志勇, 周川闽, 冯佳睿, 吴昊, 李雯. 中新生代天山隆升及其南北盆地分异与沉积环境演化[J]. 沉积学报, 2016, 34(3): 415-435. doi: 10.14027/j.cnki.cjxb.2016.03.001

引用本文:

高志勇, 周川闽, 冯佳睿, 吴昊, 李雯. 中新生代天山隆升及其南北盆地分异与沉积环境演化[J]. 沉积学报, 2016, 34(3): 415-435. doi: 10.14027/j.cnki.cjxb.2016.03.001

Citation:

GAO ZhiYong, ZHOU ChuanMin, FENG JiaRui, WU Hao, LI Wen. Relationship between the Tianshan Mountains Uplift and Depositional Environment Evolution of the Basins in Mesozoic-Cenozoic[J]. Acta Sedimentologica Sinica, 2016, 34(3): 415-435. doi: 10.14027/j.cnki.cjxb.2016.03.001

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中新生代天山隆升及其南北盆地分异与沉积环境演化

doi: 10.14027/j.cnki.cjxb.2016.03.001

作者简介:
高志勇,男,1974年出生,高级工程师,沉积学及油气储层地质,E-mail:gzybox@163.com

计量

Relationship between the Tianshan Mountains Uplift and Depositional Environment Evolution of the Basins in Mesozoic-Cenozoic

计量

目录

中新生代天山隆升及其南北盆地分异与沉积环境演化

doi: 10.14027/j.cnki.cjxb.2016.03.001

1. 中国石油勘探开发研究院实验研究中心北京 100083;

2. 提高石油采收率国家重点实验室(中国石油勘探开发研究院) 北京 100083;

3. 中国地震局北京 100036;

4. 中国地质大学地球科学与资源学院北京 100083

作者简介:
高志勇,男,1974年出生,高级工程师,沉积学及油气储层地质,E-mail:gzybox@163.com

English Abstract

Relationship between the Tianshan Mountains Uplift and Depositional Environment Evolution of the Basins in Mesozoic-Cenozoic

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中新生代天山隆升及其南北盆地分异与沉积环境演化

doi: 10.14027/j.cnki.cjxb.2016.03.001

作者简介: 高志勇,男,1974年出生,高级工程师,沉积学及油气储层地质,E-mail:gzybox@163.com

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Relationship between the Tianshan Mountains Uplift and Depositional Environment Evolution of the Basins in Mesozoic-Cenozoic

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出版历程

目录

中新生代天山隆升及其南北盆地分异与沉积环境演化

doi: 10.14027/j.cnki.cjxb.2016.03.001

1. 中国石油勘探开发研究院实验研究中心 北京 100083; 2. 提高石油采收率国家重点实验室(中国石油勘探开发研究院) 北京 100083; 3. 中国地震局 北京 100036; 4. 中国地质大学地球科学与资源学院 北京 100083

作者简介: 高志勇,男,1974年出生,高级工程师,沉积学及油气储层地质,E-mail:gzybox@163.com

English Abstract

Relationship between the Tianshan Mountains Uplift and Depositional Environment Evolution of the Basins in Mesozoic-Cenozoic

全文HTML

目录

友情链接

期刊在线

联系我们

作者简介:
高志勇,男,1974年出生,高级工程师,沉积学及油气储层地质,E-mail:gzybox@163.com

1. 中国石油勘探开发研究院实验研究中心北京 100083;

2. 提高石油采收率国家重点实验室(中国石油勘探开发研究院) 北京 100083;

3. 中国地震局北京 100036;

4. 中国地质大学地球科学与资源学院北京 100083

作者简介:
高志勇,男,1974年出生,高级工程师,沉积学及油气储层地质,E-mail:gzybox@163.com