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印支期秦岭造山活动对鄂尔多斯盆地延长组沉积特征的影响
引用本文:杨友运.印支期秦岭造山活动对鄂尔多斯盆地延长组沉积特征的影响[J].煤田地质与勘探,2004,32(5):7-9.
作者姓名:杨友运
作者单位:西安石油大学,陕西,西安,710065
基金项目:国家“十五”重点攻关项目 2 0 0 1BA6 0 5A 0 4 0 2的部分成果
摘    要:通过对鄂尔多斯盆地上三叠统延长组沉积时区域古构造活动规律、沉积地质背景研究以及延长组沉积特征和沉积相序演化规律分析,重点探讨了延长组沉积特征及沉积环境变化与印支期秦岭造山活动之间的关系,分析了印支期秦岭造山活动对盆地边界性质、盆地内延长组沉积物源、碎屑搬运和沉积机理的影响,以及沉积体系类型及沉积相带展布规律的控制作用。

关 键 词:印支期  秦岭造山活动  延长组  沉积特征  鄂尔多斯盆地
文章编号:1001-1986(2004)05-0007-03
修稿时间:2004年1月9日

Influence of Qinling Orogenic Movements in Indo-Chinese Epoch to sedimentary characteristics of Yanchang Formation in Ordos Basin
YANG You-yun.Influence of Qinling Orogenic Movements in Indo-Chinese Epoch to sedimentary characteristics of Yanchang Formation in Ordos Basin[J].Coal Geology & Exploration,2004,32(5):7-9.
Authors:YANG You-yun
Abstract:The article studies the coincident relation between the depositional characteristics & depositional environmental changes of Yanchang Formation in Ordos Basin and the Qinling Orogenic Movement in Indo-Chinese epoch. The researches are based on the area ancestral structural movement regularities, depositional geological setting, depositional features and the evolutional regularities of sedimentary context sequence in early Triassic Yanchang Formation. At the same time,it analyses the Qinling Orogenic Movement in Indo-Chinese epoch, which plays the controlling role in the basin boundary nature,the sedimentary derivation, fragmental materials transportation & depositional mechanism effects, depositional system types and depositional context belt distribution regularities of Yanchang Formation in Weibei area in the south of Ordos Basin.
Keywords:Indo-Chinese Epoch  Qinling Orogenic Movement  Yanchang Formatin  sedimentary features  Ordos Basin
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