2024 06 v.54 929-949
鄂尔多斯盆地及周缘岩相古地理与沉积演化
基金项目(Foundation):
国家自然科学基金重点项目(42230815,41630312)
邮箱(Email):
DOI:
10.16152/j.cnki.xdxbzr.2024-06-001
中文作者单位:
西北大学地质学系;陕西科技大学化学与化工学院;临沂大学生命科学学院;西安科技大学地质与环境学院;西安石油大学地球科学与工程学院;长安大学地球与资源学院;
摘要(Abstract):
鄂尔多斯盆地的沉积演化起始于中元古代，发育陆缘裂谷和陆内拗拉槽，沉积滨海相碎屑岩和潮坪相碳酸盐岩，新元古代盆地性质为大陆边缘地堑型坳陷，沉积滞留海盆碎屑岩、冰水沉积物组合及陆棚碎屑岩；早古生代寒武纪和奥陶纪的克拉通盆地主要沉积浅海碳酸盐岩，在西南缘发育沟-弧-盆体系；经过加里东运动抬升剥蚀后，开始了华北克拉通坳陷盆地的沉积演化过程，晚石炭世和早二叠世发育了陆表海沉积，早二叠世晚期—中三叠世形成了近岸碎屑湖盆沉积；中晚三叠世延长期至早白垩世，鄂尔多斯盆地最终形成，进入大型内陆差异沉积盆地的形成和发展时期，上三叠统、侏罗系和下白垩统是在鄂尔多斯盆地缓慢沉降过程中堆积的以河流-三角洲-湖泊相为特征的陆源碎屑岩系；新生代进入周边断陷发育阶段，先后发育河流-湖泊及风成沉积。这一系列沉积演化过程揭示了鄂尔多斯盆地复杂的地质历史和多样的沉积环境。
关键词(KeyWords):
克拉通边缘叠合盆地;碎屑湖盆;岩相古地理;沉积演化;鄂尔多斯盆地
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基本信息:
DOI：10.16152/j.cnki.xdxbzr.2024-06-001
中图分类号:P618.13
引用信息:
[1]李文厚,张倩,李兆雨等.鄂尔多斯盆地及周缘岩相古地理与沉积演化[J].西北大学学报(自然科学版),2024,54(06):929-949.DOI:10.16152/j.cnki.xdxbzr.2024-06-001.
基金信息:
国家自然科学基金重点项目(42230815,41630312)