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鄂尔多斯盆地怀远运动期不整合类型及其分布特征

毛丹凤 何登发 包洪平 魏柳斌 成祥 苟钧壹 石婧 许艳华

古地理学报2024,Vol.26Issue(1):119-131,13.
古地理学报2024,Vol.26Issue(1):119-131,13.DOI:10.7605/gdlxb.2024.01.004

鄂尔多斯盆地怀远运动期不整合类型及其分布特征

Distribution characteristics of different Huaiyuan unconformities in Ordos Basin

毛丹凤 1何登发 1包洪平 2魏柳斌 2成祥 1苟钧壹 1石婧 1许艳华1

作者信息

  • 1. 中国地质大学(北京)能源学院,北京 100083
  • 2. 中国石油长庆油田分公司勘探开发研究院,陕西西安 710018
  • 折叠

摘要

Abstract

The Huaiyuan Movement is an important tectonic event in the early Paleozoic of the North China Platform,resulting in a regional unconformity.Based on outcrop data,geological maps,drilling data and new seismic data,the identification marks,types and distributions of unconformities formed dur-ing the Huaiyuan movement in the Ordos Basin were analyzed.The results show that(1)sandy conglo-merate and weathered crust developed near the unconformity surface;additionally,high acoustic time,high gamma values,high content of trace elements(U,Th and K),high thorium-uranium ratios,low resistivity,and low density of logging curves occurred near the unconformity surface.The seismic response of the unconformity is characterized by a strong phase,and there are obvious differences in amplitude in-tensity,frequency and continuity in the wave groups on both sides of the unconformity.In addition,the truncation point reflections can be observed in local domain.(2)The Huaiyuan movement caused both parallel-unconformity and low-angle cutting unconformity in the basin.The former was widely distributed in the basin and its periphery areas,and the latter was distributed near the paleo-uplift in the basin.(3)The Ordos Basin and its periphery areas were affected by three stages of the Huaiyuan tectonic move-ment:during the depositional period of the Zhangxia Formation in the Middle Cambrian,uplift first oc-curred in the southeast region of the basin and then moved to the northwest direction;at the end of the Sanshanzi Formation deposition period in the late Cambrian,paleo-uplifts developed in the basin,and they were subjected to erosion;at the end of the late Cambrian,before the Ordovician Majiagou Formation was deposited,the negative drift of carbon isotopes first occurred in the bottom layer of Majiagou Forma-tion due to the influence of global sea level decline.These results provides a reference for the research of new fields of oil and gas exploration in Lower Paleozoic in the Ordos Basin.

关键词

鄂尔多斯盆地/奥陶系/削截/不整合/怀远运动

Key words

Ordos Basin/Ordovician/truncation/unconformity/Huaiyuan movement

分类

地质学

引用本文复制引用

毛丹凤,何登发,包洪平,魏柳斌,成祥,苟钧壹,石婧,许艳华..鄂尔多斯盆地怀远运动期不整合类型及其分布特征[J].古地理学报,2024,26(1):119-131,13.

基金项目

中国石油长庆油田公司科技攻关项目(编号:ZDZX2021-01)资助.Financially supported by the project of Tackling the Science and Technological Key Problems in PetroChina Changqing Oil and Gas Field Company(No.ZDZX2021-01) (编号:ZDZX2021-01)

古地理学报

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1671-1505

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