鄂尔多斯地区奥陶纪构造古地理演化与沉积充填特征<sup>&#x0002A;</sup>

doi:10.7605/gdlxb.2019.04.035

古地理学报 ›› 2019, Vol. 21 ›› Issue (4): 537-556. doi: 10.7605/gdlxb.2019.04.035

• 构造古地理学及古构造 • 下一篇

鄂尔多斯地区奥陶纪构造古地理演化与沉积充填特征^*

邵东波¹, 包洪平^1,2, 魏柳斌^1,2, 蔡郑红^1,2, 武春英^1,2, 周黎霞^1,2, 曹岩刚¹

1 中国石油长庆油田分公司,陕西西安 710018;
2 低渗透油气田勘探开发国家工程实验室,陕西西安 710018

收稿日期:2018-10-29 修回日期:2018-12-17 出版日期:2019-08-01 发布日期:2019-07-23
作者简介:邵东波,男,1966年生,高级工程师,1989年毕业于西北大学地质学系,现主要从事油气勘探地质研究和技术管理工作。E-mail:sdb_cq@petroChina.com.cn 。
基金资助:
*国家科技重大专项(编号: 2016ZX05004-006)资助

Tectonic palaeogeography evolution and sedimentary filling characteristics of the Ordovician in the Ordos area

Shao Dong-Bo¹, Bao Hong-Ping^1,2, Wei Liu-Bin^1,2, Cai Zheng-Hong^1,2, Wu Chun-Ying^1,2, Zhou Li-Xia^1,2, Cao Yan-Gang¹

1 Changqing Oil Field Branch,PetroChina,Xi’an 710018,China;
2 National Engineering Laboratory for Exploration and Development of Low Permeability Oil & Gas Field,Xi’an 710018,China

Received:2018-10-29 Revised:2018-12-17 Online:2019-08-01 Published:2019-07-23
About author:About the first author Shao Dong-Bo,born in 1966,senior engineer, graduated from Northwest University in 1989. Now he is mainly engaged in petroleum geological exploration and technical management. E-mail: sdb_cq@petroChina.com.cn.
Supported by:
Financially supported by the National Science and Technology Major Project of China(No.2016ZX05004-006)

摘要/Abstract

摘要： 鄂尔多斯地区在奥陶纪处于华北克拉通板块的西南边缘地区。由于受秦岭—祁连—贺兰三叉裂谷系开裂—聚合作用的影响,奥陶纪鄂尔多斯地区与华北克拉通已开始出现明显构造与沉积作用的分异,突出表现为奥陶纪沉积期鄂尔多斯东部大规模膏盐岩沉积层的发育。古构造分析表明鄂尔多斯地区奥陶纪总体呈现为“三隆—两坳—一古陆”的古构造分布格局;奥陶纪经历了冶里—亮甲山期的早期边部海侵、马家沟期振荡性的整体沉降海侵以及平凉—背锅山期的西南边缘快速沉陷的古地理演化过程,表现出较强的阶段性演化特征。鄂尔多斯地区奥陶纪整体的沉积充填作用具有以下重要特征: 一是受中央古隆起控制、东西向沉积分异明显;二是随时代演进,早中期以内源沉积为主,晚期则以混源或陆源碎屑沉积为主;三是西南边缘沉积巨厚,是奥陶纪最为活跃的构造沉降区。

关键词: 鄂尔多斯地区, 奥陶纪, 构造沉积分异, 古地理演化, 沉积充填, 古隆起

Abstract: The Ordos region was located in the southwestern margin of the North China Craton plate in the Ordovician. Due to the dehiscing-converging effects of the Qinling-Qilian-Helan three-armed rift system,obvious tectonic sedimentary differentiation between the Ordos area and the North China Craton had begun to occur in Ordovician. The prominent expression is the large-scale development of evaporite deposits in the eastern part of Ordos area during the Ordovician depositional period. Palaeotectonics analysis shows that the Ordos area was generally characterized by the palaeotectonics distribution pattern of “three uplifts-two depressions-one archicontinent” in the Ordovician. During the Ordovician,it experienced sevaral palaeogeography evolution processes, respectively the marginal transgression in the early Yeli-Liangjiashan period,the oscillating whole-subsidence transgression in the Majiagou period,and the southwestern marginal fast subsidence in the Pingliang-Beiguoshan period, which is characterized by a strong evolution. The sedimentary-filling effect of the Ordos area in the Ordovician has the following important features: Firstly,being controlled by the central palaeo-uplift,the east-west sedimentary differentiation is obvious; secondly,with the evolution of the times,the inner-source sedimentation is dominant in the early and mid-term,while the mixed source or terrigenous clastic deposition is dominant in the late stage; thirdly,the deposits in the southwestern margins are hugely thick,where the structural subsidence is the most active during the Ordovician.

Key words: Ordos area, Ordovician, tectonic sedimentary differentiation, palaeogeographic evolution, sedimentary filling, palaeouplift

中图分类号:

P512.2

邵东波, 包洪平, 魏柳斌, 蔡郑红, 武春英, 周黎霞, 曹岩刚. 鄂尔多斯地区奥陶纪构造古地理演化与沉积充填特征^*[J]. 古地理学报, 2019, 21(4): 537-556.

Shao Dong-Bo, Bao Hong-Ping, Wei Liu-Bin, Cai Zheng-Hong, Wu Chun-Ying, Zhou Li-Xia, Cao Yan-Gang. Tectonic palaeogeography evolution and sedimentary filling characteristics of the Ordovician in the Ordos area[J]. JOPC, 2019, 21(4): 537-556.

http://www.gdlxb.cn/CN/Y2019/V21/I4/537

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鄂尔多斯地区奥陶纪构造古地理演化与沉积充填特征^*

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鄂尔多斯地区奥陶纪构造古地理演化与沉积充填特征*

Tectonic palaeogeography evolution and sedimentary filling characteristics of the Ordovician in the Ordos area

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鄂尔多斯地区奥陶纪构造古地理演化与沉积充填特征^*