| 湘黔桂相邻区新元古代820～635Ma时期裂谷盆地充填序列与地层格架 |
| |
| 引用本文： | 陈建书,戴传固,彭成龙,王敏,卢定彪,王雪,华骆珊.湘黔桂相邻区新元古代820～635Ma时期裂谷盆地充填序列与地层格架[J].中国地质,2016(3):899-920. |
| |
| 作者姓名： | 陈建书 戴传固 彭成龙 王敏 卢定彪 王雪 华骆珊 |
| |
| 作者单位： | 贵州省地质调查院, 贵州 贵阳 550005,贵州省地质调查院, 贵州 贵阳 550005,贵州省地质调查院, 贵州 贵阳 550005,贵州省地质调查院, 贵州 贵阳 550005,贵州省地质调查院, 贵州 贵阳 550005,贵州省地质调查院, 贵州 贵阳 550005,贵州省地质调查院, 贵州 贵阳 550005 |
| |
| 基金项目： | 中国地质调查局基础地质综合研究项目(1212011120108,1212011121106)资助。 |
| |
| 摘 要： | 湘黔桂相邻区发育一套序列完整、界面清楚的武陵造山运动不整合面之上至震旦纪(820~635 Ma)时期的裂谷盆地沉积地层。通过详细的区域岩石地层划分与对比,结合年代学研究成果,显示其时空展布格局完整,充填序列连续,划分标志清楚,完全可以划分对比。在此基础上建立了其地层格架,为扬子古大陆周缘新元古代820~635 Ma时期地层划分对比研究提供了详实的资料,亦为中国前寒武系新元古代地层划分对比及国际新元古代研究提供了新的资料成果。
|
| 关 键 词： | 地层划分对比 充填序列 地层格架 新元古代 湘黔桂邻区 |
| 收稿时间： | 2015/9/30 0:00:00 |
| 修稿时间： | 2016/3/16 0:00:00 |
The filling sequence and stratigraphic framework of rift basin during the Neoproterozoic 820-635 Ma in Hunan, Guizhou and Guangxi |
| |
| CHEN Jian-shu,DAI Chuan-gu,PENG Cheng-long,WANG Min,LU Ding-biao,WANG Xue-hua and LUO Shan.The filling sequence and stratigraphic framework of rift basin during the Neoproterozoic 820-635 Ma in Hunan, Guizhou and Guangxi[J].Chinese Geology,2016(3):899-920. |
| |
| Authors: | CHEN Jian-shu DAI Chuan-gu PENG Cheng-long WANG Min LU Ding-biao WANG Xue-hua and LUO Shan |
| |
| Institution: | Geological Survey of Guizhou Province, Guiyang 550005, Guizhou, China,Geological Survey of Guizhou Province, Guiyang 550005, Guizhou, China,Geological Survey of Guizhou Province, Guiyang 550005, Guizhou, China,Geological Survey of Guizhou Province, Guiyang 550005, Guizhou, China,Geological Survey of Guizhou Province, Guiyang 550005, Guizhou, China,Geological Survey of Guizhou Province, Guiyang 550005, Guizhou, China and Geological Survey of Guizhou Province, Guiyang 550005, Guizhou, China |
| |
| Abstract: | A set of Neoproterozoic(820-635 Ma)sedimentary strata are developed in Hunan, Guizhou and Guangxi, which occur above the Wuling Movement and below the Zhendan System, serving as the formation of lift basin with the well developed succession and clear sedimentary boundary. The stratigraphic system, according to the stratigraphical division and correlation of the regional rock and strata in combination with the recent results of chronology, shows a completed distribution and evolution, successive strata, and a clear division mark; it therefore can be completely divided and contrasted. On the basis of the stratigraphic division and correlation, the authors formulated a stratigraphic framework, which presents a set of detailed and accurate data for studying the stratigraphic division and correlation of the Neoproterozoic ( 820- 635 Ma) sedimentary strata in the Yangtze Paleocontinent, and also offers the new resultant data for studying the Precambrian including the Neoproterozoic in China. |
| |
| Keywords: | stratigraphic division and correlation filling sequence stratigraphic framework Neoproterozoic Hunan Guizhou and Guangxi |
| 本文献已被 CNKI 等数据库收录！ |
| 点击此处可从《中国地质》浏览原始摘要信息 |
| 点击此处可从《中国地质》下载免费的PDF全文 |
|
