| 黔西北丁台地区下寒武统清虚洞组风暴沉积的发现及其意义 |
| |
| 引用本文： | 郑斌嵩,牟传龙,梁薇,陈超,徐鹏辉,孙小勇.黔西北丁台地区下寒武统清虚洞组风暴沉积的发现及其意义[J].沉积学报,2016,34(3):478-486. |
| |
| 作者姓名： | 郑斌嵩 牟传龙 梁薇 陈超 徐鹏辉 孙小勇 |
| |
| 作者单位： | 1.中国地质大学(北京)地球科学与资源学院 北京 100083; |
| |
| 基金项目： | 国家科技重大专项(2008ZX05043-005)，中国地质调查局项目(1212010916060;12120115004301)，国家自然科学基金项目(41302093)National Science and Technology Major Project |
| |
| 摘 要： | 黔西北遵义丁台剖面下寒武统龙王庙阶清虚洞组的底部和中部发育两套具有不同沉积特征的风暴沉积,与同时期风暴沉积多发现于黔东湘西台缘区不同,研究在黔西北台地内部发现该时期风暴沉积。其底部风暴沉积段发育侵蚀底面、粗粒滞留沉积、丘-洼状交错层理、沙纹层理和泥晶灰岩背景沉积,共识别出三种类型的风暴沉积序列,其沉积特征指示其形成于正常浪基面与风暴浪基面之间的中缓坡环境,而中部风暴沉积段则发育粗粒滞留沉积、粒序层理、沙纹层理和具鸟眼构造的藻屑灰岩背景沉积,可识别出四种类型的风暴沉积序列,其沉积特征指示其形成于浪基面之上的浅水潮坪环境。本剖面上下两段形成于不同沉积背景的风暴沉积的发现不仅丰富了我们对风暴沉积的认识,更为重要的是为研究早寒武世龙王庙期扬子地台的古纬度及古板块演化、地层等时对比和古地理演化提供了极有价值的资料。
|
| 关 键 词： | 黔西北 丁台剖面 下寒武统 清虚洞组 风暴沉积 |
| 收稿时间： | 2015-06-15 |
Discovery and Significance of the Storm Deposit within the Lower Cambrian Qingxudong Formation in the Dingtai Area,Northwestern Guizhou |
| |
| ZHENG BinSong,MOU ChuanLong,LIANG Wei,CHEN Chao,XU PengHui,SUN XiaoYong.Discovery and Significance of the Storm Deposit within the Lower Cambrian Qingxudong Formation in the Dingtai Area,Northwestern Guizhou[J].Acta Sedimentologica Sinica,2016,34(3):478-486. |
| |
| Authors: | ZHENG BinSong MOU ChuanLong LIANG Wei CHEN Chao XU PengHui SUN XiaoYong |
| |
| Institution: | 1.School of Earth Sciences and Resources, China University of Geosciences(Beijing), Beijing 100083, China;2.Chendu Institute of Geology and Mineral Resources, Chengdu 610081, China;3.Key Laboratory for Sedimentary Basin and Oil and Gas Resources, Ministy of Land and Resources, Chengdu 610081, China;4.Chinese Academy of Geological Sciences, Beijing 100037, China;5.Chengdu University of Technology, Chengdu 610059, China |
| |
| Abstract: | Two sets of storm deposits, with different sedimentary characteristics, were found at the bottom and the middle of Qingxudong Formation(Lungwangmiaoan Stage, Lower Cambrian)of the Dingtai section, Zunyi, northwestern Guizhou province, which are different from the discovery of the storm deposits that were found mostly at the platform margin in eastern Hunan and western Guizhou. It was the first time that we found storm deposits at the interior of the Yangtze platform in northwestern Guizhou at the same stage. At the bottom, we found erosion surface, coarse lag deposit, hummocky-sunken cross-stratification, ripple bedding, and micrite limestone, which represents the background deposit, and we can recognize three types of storm deposit sequences, and its sedimentary characteristics indicate that it was deposited at middle ramp, between the wave base and the storm wave base. At the middle, we found coarse lag deposit, graded bedding and ripple bedding, and the background deposit is algal clast limestone which develops bird-eye structure, and there are four types of storm deposit sequences that we can recognize, and its sedimentary characteristics indicate that it was deposited at shallow water tidal flat, above the wave base. The discovery of this two sets of storm deposits, which deposited at different settings, not only enrich our understanding of storm deposit, but more impotant is that it can provide us valuable infomation for our study on the evolution of paleolatitude and paleoplate, the isochronostratigraphic correlation and the evolution of paleogeography of the Yangtze platform in the Lungwangmiaoan Stage, Lower Cambrian. |
| |
| Keywords: | northwestern Guizhou Dingtai section Lower Cambrian Qingxudong Formation storm deposit |
| 本文献已被 CNKI 万方数据 等数据库收录！ |
| 点击此处可从《沉积学报》浏览原始摘要信息 |
| 点击此处可从《沉积学报》下载免费的PDF全文 |
|
