塔里木盆地志留纪沉积层序构成及充填响应特征

施振生

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塔里木盆地志留纪沉积层序构成及充填响应特征

施振生

文章导航 > 沉积学报 > 2007 > 25(3): 401-408

施振生. 塔里木盆地志留纪沉积层序构成及充填响应特征[J]. 沉积学报, 2007, 25(3): 401-408.

引用本文:

施振生. 塔里木盆地志留纪沉积层序构成及充填响应特征[J]. 沉积学报, 2007, 25(3): 401-408.

SHI Zhensheng. Depositional Sequence and Filling Response Characteristics ofSilurian in Tarim Basin[J]. Acta Sedimentologica Sinica, 2007, 25(3): 401-408.

Citation:

SHI Zhensheng. Depositional Sequence and Filling Response Characteristics ofSilurian in Tarim Basin[J]. Acta Sedimentologica Sinica, 2007, 25(3): 401-408.

施振生. 塔里木盆地志留纪沉积层序构成及充填响应特征[J]. 沉积学报, 2007, 25(3): 401-408.

引用本文:

施振生. 塔里木盆地志留纪沉积层序构成及充填响应特征[J]. 沉积学报, 2007, 25(3): 401-408.

SHI Zhensheng. Depositional Sequence and Filling Response Characteristics ofSilurian in Tarim Basin[J]. Acta Sedimentologica Sinica, 2007, 25(3): 401-408.

Citation:

SHI Zhensheng. Depositional Sequence and Filling Response Characteristics ofSilurian in Tarim Basin[J]. Acta Sedimentologica Sinica, 2007, 25(3): 401-408.

塔里木盆地志留纪沉积层序构成及充填响应特征

施振生

中国石油勘探开发研究院廊坊分院河北廊坊 065007

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施振生

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Depositional Sequence and Filling Response Characteristics ofSilurian in Tarim Basin

SHI Zhensheng

Gas Department,Langfang Branch,Research Institute of Petroleum Exploration and Development,CNPC,Langfang,Hebei 065007

More Information

Corresponding author: SHI Zhensheng

摘要

摘要: 塔里木盆地志留系是由角度不整合面所限定的一个区域性（二级）的沉积层序，其内可划分出5个三级沉积层序。总体上显示一个从水进到水退的沉积旋回，可识别出曲流河三角洲—辫状河三角洲、滨外陆棚及较深水盆地、无障壁碎屑滨岸—无障壁碎屑潮坪沉积体系组合，它们代表了二级沉积层序中相对低位、海侵和高位的3个沉积体系组合。研究区构造、沉积、古生物和古气候资料表明，层序1底界面和层序5顶界面是塔里木周缘板块构造挤压、盆地隆升作用的结果；层序2底界面是周缘板块强烈挤压、盆地挠曲下降作用结果，同期全球海平面快速上升；层序3、层序4和层序5的底界面是在构造作用稳定、全球海平面下降背景之上由相对海平面次一级旋回变化形成的，是古气候变化、沉积物供给及构造沉降共同作用的结果。
- 志留纪 /
- 沉积层序 /
- 古气候 /
- 充填响应 /
- 塔里木盆地
Abstract: Silurian in Tarim Basin，bounded at the top and base by widely spread regional unconformities，can be divided into 1 secondorder sequence and 5 thirdorder sequences. Three kinds of depositional system assemblages，which represent lowstand systems tract，transgressive systems tract，and highstand systems of the secondorder sequence，are identified in Silurian of Tarim Basin, namely, assemblage of meandering river delta and braided river delta depositional systems，assemblage of offshore and slightly deepwater basin depositional systems, and assemblage of clastic coastal depositional system with no barriers and clastic tidal depositional system with no barriers. Based on the integrated analysis of data of tectonics，sedimentology，palaeontology and palaeoclimatology，the base boundary of sequence 1 and top boundary of sequence 5 are thought to be originated from the pressure of peripheral plates and uplift of basin base. The bottom boundary of sequence 2 belongs to tectonically compressed unconformity that originates from the pressure of plates and decline of basin base. The bottom boundary of sequence 3, sequence 4 and sequence 5 results from integrated effect of change of climate, sediment source and tectonic activity under falling global eustacy. 
- Silurian /
- depositional sequence /
- palaeoclimate /
- filling response /
- Tarim Basin

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[1]	陈国辉, 李超, 李宏卫, 查凯婕. 粤北丹霞盆地上白垩统陆相红层地球化学特征及其古气候意义 . 沉积学报, 2025, (): -. doi: 10.14027/j.issn.1000-0550.2024.118
[2]	周敏, 李祥辉, 王旌羽. 四川盆地东北部中—晚侏罗世沉积环境与古气候 . 沉积学报, 2024, 42(3): 1003-1015. doi: 10.14027/j.issn.1000-0550.2022.079
[3]	李相博, 朱如凯, 惠潇, 苏明军, 邱振, 黄军平, 张艳, 王菁, 刘化清, 李士祥, 李树同, 杨占龙, 郭精义. 晚三叠世卡尼期梅雨事件（CPE）在陆相盆地中的沉积学响应 . 沉积学报, 2023, 41(2): 511-526. doi: 10.14027/j.issn.1000-0550.2022.008
[4]	谢巍, 李一凡, 刘旺威. 塔里木盆地东北缘下寒武统泥页岩古气候与物源背景研究 . 沉积学报, 2023, 41(4): 1240-1256. doi: 10.14027/j.issn.1000-0550.2021.159
[5]	冯轩, 吴永华, 杨宝菊, 单新, 刘季花. 冲绳海槽西南端1.3ka以来异重流沉积记录及其古气候响应 . 沉积学报, 2021, 39(3): 739-750. doi: 10.14027/j.issn.1000-0550.2020.018
[6]	陈留勤, 李鹏程, 郭福生, 刘鑫, 李馨敏. 粤北丹霞盆地晚白垩世丹霞组沉积相及古气候意义 . 沉积学报, 2019, 37(1): 17-29. doi: 10.14027/j.issn.1000-0550.2018.118
[7]	陈留勤, 刘鑫, 李鹏程. 古土壤:沉积环境和古气候变化的灵敏指针 . 沉积学报, 2018, 36(3): 510-520. doi: 10.14027/j.issn.1000-0550.2018.054
[8]	王玥铭, 窦衍光, 李军, 徐景平, 蔡峰, 温珍河, 赵京涛, 陈晓辉. 16 ka以来冲绳海槽中南部沉积物物源演化及其对古气候的响应 . 沉积学报, 2018, 36(6): 1157-1168. doi: 10.14027/j.issn.1000-0550.2018.102
[9]	伏美燕, 李娜, 黄茜, 刘磊. 滨岸-浅海混合沉积对海平面与气候变化的响应——以塔里木盆地巴麦地区石炭系为例 . 沉积学报, 2017, 35(6): 1110-1120. doi: 10.14027/j.cnki.cjxb.2017.06.003
[10]	王尹, 李祥辉, 周勇, 刘玲. 南雄盆地晚白垩世—古新世陆源沉积组份变化的古气候指示 . 沉积学报, 2015, 33(1): 116-123. doi: 10.14027/j.cnki.cjxb.2015.01.012
[11]	. 珠江口盆地番禺天然气区东南缘坡折带韩江组中段沉积层序与岩性地层圈闭研究 . 沉积学报, 2013, 31(6): 1081-1087.
[12]	徐兆辉. 古气候恢复及其对沉积的控制作用——以四川盆地上三叠统须家河组为例 . 沉积学报, 2011, 29(2): 235-244.
[13]	孟昌. 塔里木盆地西北缘海相白垩系—古近系界线沉积物环境指标研究 . 沉积学报, 2011, 29(2): 245-254.
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[20]	费富安. 对苏北含油盆地下第三系古环境和古气候的探讨 . 沉积学报, 1988, 6(1): 21-28.

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文章访问数: 1903
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塔里木盆地志留纪沉积层序构成及充填响应特征

施振生

中国石油勘探开发研究院廊坊分院河北廊坊 065007

通讯作者: 施振生

收稿日期: 1900-01-01
修回日期: 1900-01-01
刊出日期: 2007-06-10

关键词:

志留纪 /

沉积层序 /

古气候 /

充填响应 /

塔里木盆地

摘要: 塔里木盆地志留系是由角度不整合面所限定的一个区域性（二级）的沉积层序，其内可划分出5个三级沉积层序。总体上显示一个从水进到水退的沉积旋回，可识别出曲流河三角洲—辫状河三角洲、滨外陆棚及较深水盆地、无障壁碎屑滨岸—无障壁碎屑潮坪沉积体系组合，它们代表了二级沉积层序中相对低位、海侵和高位的3个沉积体系组合。研究区构造、沉积、古生物和古气候资料表明，层序1底界面和层序5顶界面是塔里木周缘板块构造挤压、盆地隆升作用的结果；层序2底界面是周缘板块强烈挤压、盆地挠曲下降作用结果，同期全球海平面快速上升；层序3、层序4和层序5的底界面是在构造作用稳定、全球海平面下降背景之上由相对海平面次一级旋回变化形成的，是古气候变化、沉积物供给及构造沉降共同作用的结果。

English Abstract

Depositional Sequence and Filling Response Characteristics ofSilurian in Tarim Basin

SHI Zhensheng

Gas Department,Langfang Branch,Research Institute of Petroleum Exploration and Development,CNPC,Langfang,Hebei 065007

Corresponding author: SHI Zhensheng

Received Date: 1900-01-01
Rev Recd Date: 1900-01-01
Publish Date: 2007-06-10

Keywords:

Abstract: Silurian in Tarim Basin，bounded at the top and base by widely spread regional unconformities，can be divided into 1 secondorder sequence and 5 thirdorder sequences. Three kinds of depositional system assemblages，which represent lowstand systems tract，transgressive systems tract，and highstand systems of the secondorder sequence，are identified in Silurian of Tarim Basin, namely, assemblage of meandering river delta and braided river delta depositional systems，assemblage of offshore and slightly deepwater basin depositional systems, and assemblage of clastic coastal depositional system with no barriers and clastic tidal depositional system with no barriers. Based on the integrated analysis of data of tectonics，sedimentology，palaeontology and palaeoclimatology，the base boundary of sequence 1 and top boundary of sequence 5 are thought to be originated from the pressure of peripheral plates and uplift of basin base. The bottom boundary of sequence 2 belongs to tectonically compressed unconformity that originates from the pressure of plates and decline of basin base. The bottom boundary of sequence 3, sequence 4 and sequence 5 results from integrated effect of change of climate, sediment source and tectonic activity under falling global eustacy. 

施振生. 塔里木盆地志留纪沉积层序构成及充填响应特征[J]. 沉积学报, 2007, 25(3): 401-408.

引用本文:

施振生. 塔里木盆地志留纪沉积层序构成及充填响应特征[J]. 沉积学报, 2007, 25(3): 401-408.

SHI Zhensheng. Depositional Sequence and Filling Response Characteristics ofSilurian in Tarim Basin[J]. Acta Sedimentologica Sinica, 2007, 25(3): 401-408.

Citation:

SHI Zhensheng. Depositional Sequence and Filling Response Characteristics ofSilurian in Tarim Basin[J]. Acta Sedimentologica Sinica, 2007, 25(3): 401-408.

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塔里木盆地志留纪沉积层序构成及充填响应特征

通讯作者:
施振生

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Depositional Sequence and Filling Response Characteristics ofSilurian in Tarim Basin

Corresponding author: SHI Zhensheng

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目录

塔里木盆地志留纪沉积层序构成及充填响应特征

中国石油勘探开发研究院廊坊分院河北廊坊 065007

通讯作者: 施振生

English Abstract

Depositional Sequence and Filling Response Characteristics ofSilurian in Tarim Basin

Gas Department,Langfang Branch,Research Institute of Petroleum Exploration and Development,CNPC,Langfang,Hebei 065007

Corresponding author: SHI Zhensheng

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塔里木盆地志留纪沉积层序构成及充填响应特征

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Depositional Sequence and Filling Response Characteristics ofSilurian in Tarim Basin

Corresponding author: SHI Zhensheng

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出版历程

目录

塔里木盆地志留纪沉积层序构成及充填响应特征

中国石油勘探开发研究院廊坊分院 河北廊坊 065007

通讯作者: 施振生

English Abstract

Depositional Sequence and Filling Response Characteristics ofSilurian in Tarim Basin

Gas Department,Langfang Branch,Research Institute of Petroleum Exploration and Development,CNPC,Langfang,Hebei 065007

Corresponding author: SHI Zhensheng

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施振生

中国石油勘探开发研究院廊坊分院河北廊坊 065007