|本期目录/Table of Contents|

[1]侯林君,陈洪德*,罗林军,等.鄂尔多斯盆地前寒武纪末期古地貌恢复及其对烃源岩的控制作用[J].地球科学与环境学报,2019,41(04):475-490.
 HOU Lin-jun,CHEN Hong-de*,LUO Lin-jun,et al.Reconstruction of Late Precambrian Palaeogeomorphology in Ordos Basin, China and Its Control on Source Rocks[J].Journal of Earth Sciences and Environment,2019,41(04):475-490.
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鄂尔多斯盆地前寒武纪末期古地貌恢复及其对烃源岩的控制作用(PDF)
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《地球科学与环境学报》[ISSN:1672-6561/CN:61-1423/P]

卷:
第41卷
期数:
2019年第04期
页码:
475-490
栏目:
基础地质与矿产地质
出版日期:
2019-07-15

文章信息/Info

Title:
Reconstruction of Late Precambrian Palaeogeomorphology in Ordos Basin, China and Its Control on Source Rocks
文章编号:
1672-6561(2019)04-0475-16
作者:
侯林君12陈洪德12*罗林军3张成弓12赵俊兴12苏中堂12
沉积地质研究院,四川 成都 610059; 3. 中国石油长庆油田分公司第一采油厂,陕西 延安 717400)
Author(s):
HOU Lin-jun12 CHEN Hong-de12* LUO Lin-jun3 ZHANG Cheng-gong12 ZHAO Jun-xing12 SU Zhong-tang12
(1. State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation, Chengdu University of Technology, Chengdu 610059, Sichuan, China; 2. Institute of Sedimentary Geology, Chengdu University of Technology, Chengdu 610059, Sichuan, China; 3. No.1 Oil Recovery Plant, Changqing Oilfield Company, PetroChina, Yan’an 717400, Shaanxi, China)
关键词:
古地貌 前寒武纪 层序 标志层 印模法 古地质图 烃源岩 鄂尔多斯盆地
Keywords:
paleogeomorphology Precambrian sequence marker bed impression method paleogeological map source rock Ordos Basin
分类号:
P531; P931
DOI:
-
文献标志码:
A
摘要:
鄂尔多斯盆地前寒武纪末期古地貌控制着后期沉积体系的空间配置与古地理展布。通过野外剖面、岩芯分析、测井数据等建立鄂尔多斯盆地寒武系层序地层格架; 选取寒武纪SS1最大海泛面(徐庄组沉积晚期地层)为标志层,通过残余厚度印模法,并结合古地质图分析,对研究区前寒武纪进行古地貌恢复,明确了前寒武纪沉积背景、构造格局及物源方向。总体上,前寒武纪鄂尔多斯盆地南、北濒临秦祁海和兴蒙海,东、西被贺兰和晋豫陕坳拉槽所夹持,古地貌东北高、西南低,受秦祁海影响最大,可将其划分为3个古构造地貌单元:高地剥蚀区、受古构造控制形成的坳陷区以及处于剥蚀与沉积过渡地带的斜坡阶地区。通过研究前寒武纪末期古地貌与寒武纪早期烃源岩分布认为,拉张活动背景下的坳陷带以及斜坡带是鄂尔多斯盆地寒武纪早期烃源岩发育的有利区块,前寒武纪古地貌格局影响了寒武纪早期烃源岩发育与分布。恢复古地貌形态对于揭示物源供给,研究沉积物搬运、平面和纵向展布特征,探究沉积、沉降中心的迁移规律,以及进一步揭示生储盖组合和分布具有重大意义。
Abstract:
Late Precambrian paleogeomorphology in Ordos Basin controls spatial and paleogeographic distributions of the subsequent sedimentary system. Cambrian sequence stratigraphic framework in Ordos Basin was established by outcrop observation, core description and logging data. The largest sea surface of Cambrian SS1(late sedimentary strata of Xuzhuang Formation)was selected as the marker bed; combined with the means of the residual thickness impression method and paleogeological map analysis, the Precambrian paleogeomorphology in the area was reconstructed; meanwhile, the sedimentary background, tectonic framework and provenance direction in Precambrian were defined. Generally, Ordos Basin in Precambrian is bordered by Qinling-Qilian Sea and Xing’an-Mongolian Sea in the north and south, and is clamped by Helan aulacogen and Shanxi-Henan-Shaanxi aulacogen in the east and west. The palaeogeomorphology in Ordos Basin is characterized by the higher in the northeast and the lower in the southwest, and greatly affected by Qinling-Qilian Sea; and it can be divided into three palaeotectonic geomorphic units, including the high-land denudation area, the depression area controlled by palaeotectonics and the slope terrace located in the transition zone between denudation and deposition. By studying Late Precambrian paleogeomorphology and the distribution of Early Cambrian source rocks, it is considered that depression belts in the background of tensile activity and slope belts are favorable blocks for the development of Early Cambrian source rocks in Ordos Basin, and the Precambrian palaeogeomorphology pattern affects the development and distribution of Early Cambrian source rocks. The reconstruction of paleogeomorphology is of great significance for revealing the source supply, studying the sediment transport and characteristics of horizontal and vertical distributions, exploring the migration law of sedimentation and subsidence centers, and further revealing the source-reservoir-cap assemblage and distribution.

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备注/Memo

备注/Memo:
收稿日期:2019-03-18; 修回日期:2019-04-23投稿网址:http://jese.chd.edu.cn/
基金项目:国家自然科学基金项目(41602107); 油气藏地质及开发工程国家重点实验室开放基金项目(PLC20180307)
作者简介:侯林君(1993-),男,山西忻州人,理学硕士研究生,E-mail:723263837@qq.com。
*通讯作者:陈洪德(1956-),男,四川资中人,教授,博士研究生导师,理学博士,E-mail:chd@cdut.edu.cn。
更新日期/Last Update: 2019-07-11