| 内蒙古扎兰屯格根敖包组一段沉积岩层序地层特征 |
| |
| 引用本文： | 吴桐,李伟,司秋亮,唐振,马永非.内蒙古扎兰屯格根敖包组一段沉积岩层序地层特征[J].地质与资源,2016,25(3):218-222. |
| |
| 作者姓名： | 吴桐 李伟 司秋亮 唐振 马永非 |
| |
| 作者单位： | 1. 吉林大学 地球科学学院, 吉林 长春 130026;2. 中国地质调查局 沈阳地质调查中心(沈阳地质矿产研究所), 辽宁 沈阳 110034 |
| |
| 基金项目： | 中国地质调查局“内蒙古1/5万大呼勒气沟等四幅区域地质调查”(编号1212011120665)，“松辽外围西部盆地群油气基础地质调查”(编号12120115001001) |
| |
| 摘 要： | 扎兰屯哈拉口子北山上石炭统—下二叠统格根敖包组一段沉积岩非常发育,为一套正常陆源碎屑沉积岩组合.根据岩石组合特征、组构、岩层垂向变化规律、沉积环境变化等分析,本区格根敖包组一段沉积岩自下而上可划分为1个Ⅱ级层序,3个Ⅲ级层序及7个Ⅳ级层序.对其进行层序地层学等方面的研究,为大兴安岭地区晚古生代沉积盆地层序地层的研究提供一定的参考.
|
| 关 键 词： | 格根敖包组一段 层序地层 沉积地层 扎兰屯 内蒙古 |
| 收稿时间： | 2015-12-30 |
SEQUENCE STRATIGRAPHY OF THE FIRST MEMBER OF GEGENAOBAO FORMATION IN ZHALANTUN AREA,INNER MONGOLIA |
| |
| WU Tong,LI Wei,SI Qiu-liang,TANG Zhen,MA Yong-fei.SEQUENCE STRATIGRAPHY OF THE FIRST MEMBER OF GEGENAOBAO FORMATION IN ZHALANTUN AREA,INNER MONGOLIA[J].Geology and Resources,2016,25(3):218-222. |
| |
| Authors: | WU Tong LI Wei SI Qiu-liang TANG Zhen MA Yong-fei |
| |
| Institution: | 1. College of Earth Sciences, Jilin University, Changchun 130061, China;2. Shenyang Institute of Geology and Mineral Resources, CGS, Shenyang 110034, China |
| |
| Abstract: | A set of normal terrigenous clastic sedimentary rocks of the first member of Gegenaobao Formation, Upper Carboniferous-Lower Permian, is well developed in Zhalatun area, Inner Mongolia. Base on the analysis of the rock assemblage, composition, vertical variation of strata and sedimentary environment change, the sedimentary rocks of Gegenaobao Formation may be subdivided into one Grade Ⅱ sequence, including three Grade Ⅲ sequences and seven Grade IV sequences. Study on the sequence stratigraphy provides a valuable reference for the Late Paleozoic sedimentary basin formation in Daxinganling region. |
| |
| Keywords: | first member of Gegenaobao Formation sequence stratigraphy sedimentary strata Zhalantun Inner Mongolia |
| 本文献已被 CNKI 万方数据 等数据库收录！ |
| 点击此处可从《地质与资源》浏览原始摘要信息 |
| 点击此处可从《地质与资源》下载免费的PDF全文 |
|
