W. Li, Shiguo Wu, Xiujuan Wang, Dawei Wang, F. Zhao
{"title":"琼东南盆地中央峡谷上新世块体搬运沉积的地震特征与分布:琼东南盆地中央峡谷上新世块体搬运沉积的地震特征与分布","authors":"W. Li, Shiguo Wu, Xiujuan Wang, Dawei Wang, F. Zhao","doi":"10.3724/SP.J.1140.2013.02009","DOIUrl":null,"url":null,"abstract":"2D/3D seismic data and coherence of 3D seismic data in the deepwater area of Qiongdongnan Basin reveal the occurrence of multi-stage mass transport deposits(MTDs) in the Central Canyon of the basin.The MTDs of this region consist of three units,namely the headwall domain,the translational domain and the toe domain characterized by different seismic characteristics.Being regarded as an important part of deepwater deposition in the Central Canyon of Qiongdongnan Basin since Neogene,the large-scale MTDs have an important effect on the spatial distribution of sediment in the deepwater basin.The Pliocene MTDs are distributed in an area of 300 km2,with a thickness up to 240 m in a fan shape in planar distribution.The rapid sedimentary discharge and active tectonic movement may be the main reasons for the development of the MTDs in Central Canyon of Qiongdongnan Basin..In addition,earthquakes and fluctuation of sea level have a significant effect on the formation of the MTDs.","PeriodicalId":18188,"journal":{"name":"海洋地质与第四纪地质","volume":"33 1","pages":"9-16"},"PeriodicalIF":0.0000,"publicationDate":"2014-03-06","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"2","resultStr":"{\"title\":\"SEISMIC CHARACTERISTICS AND DISTRIBUTION OF PLIOCENE MASS TRANSPORT DEPOSITS IN CENTRAL CANYON OF QIONGDONGNAN BASIN: SEISMIC CHARACTERISTICS AND DISTRIBUTION OF PLIOCENE MASS TRANSPORT DEPOSITS IN CENTRAL CANYON OF QIONGDONGNAN BASIN\",\"authors\":\"W. Li, Shiguo Wu, Xiujuan Wang, Dawei Wang, F. Zhao\",\"doi\":\"10.3724/SP.J.1140.2013.02009\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"2D/3D seismic data and coherence of 3D seismic data in the deepwater area of Qiongdongnan Basin reveal the occurrence of multi-stage mass transport deposits(MTDs) in the Central Canyon of the basin.The MTDs of this region consist of three units,namely the headwall domain,the translational domain and the toe domain characterized by different seismic characteristics.Being regarded as an important part of deepwater deposition in the Central Canyon of Qiongdongnan Basin since Neogene,the large-scale MTDs have an important effect on the spatial distribution of sediment in the deepwater basin.The Pliocene MTDs are distributed in an area of 300 km2,with a thickness up to 240 m in a fan shape in planar distribution.The rapid sedimentary discharge and active tectonic movement may be the main reasons for the development of the MTDs in Central Canyon of Qiongdongnan Basin..In addition,earthquakes and fluctuation of sea level have a significant effect on the formation of the MTDs.\",\"PeriodicalId\":18188,\"journal\":{\"name\":\"海洋地质与第四纪地质\",\"volume\":\"33 1\",\"pages\":\"9-16\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"2014-03-06\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"2\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"海洋地质与第四纪地质\",\"FirstCategoryId\":\"1089\",\"ListUrlMain\":\"https://doi.org/10.3724/SP.J.1140.2013.02009\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"海洋地质与第四纪地质","FirstCategoryId":"1089","ListUrlMain":"https://doi.org/10.3724/SP.J.1140.2013.02009","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
SEISMIC CHARACTERISTICS AND DISTRIBUTION OF PLIOCENE MASS TRANSPORT DEPOSITS IN CENTRAL CANYON OF QIONGDONGNAN BASIN: SEISMIC CHARACTERISTICS AND DISTRIBUTION OF PLIOCENE MASS TRANSPORT DEPOSITS IN CENTRAL CANYON OF QIONGDONGNAN BASIN
2D/3D seismic data and coherence of 3D seismic data in the deepwater area of Qiongdongnan Basin reveal the occurrence of multi-stage mass transport deposits(MTDs) in the Central Canyon of the basin.The MTDs of this region consist of three units,namely the headwall domain,the translational domain and the toe domain characterized by different seismic characteristics.Being regarded as an important part of deepwater deposition in the Central Canyon of Qiongdongnan Basin since Neogene,the large-scale MTDs have an important effect on the spatial distribution of sediment in the deepwater basin.The Pliocene MTDs are distributed in an area of 300 km2,with a thickness up to 240 m in a fan shape in planar distribution.The rapid sedimentary discharge and active tectonic movement may be the main reasons for the development of the MTDs in Central Canyon of Qiongdongnan Basin..In addition,earthquakes and fluctuation of sea level have a significant effect on the formation of the MTDs.
期刊介绍:
Marine Geology and Quaternary Geology launched in 1981 is a bimonthly academic journal sponsored by Qingdao Institute of Marine Geology, China Geological Survey, and published by the Science Press, China.The journal aims to publish original, cutting-edge, and explorative scientific results in the field of marine geology and sea-land Quaternary geology. The journal focus on reporting the latest research achievements supported by National Natural Science Foundation Project, National Key Project and International Cooperation Project, with priority to the results in China seas, global ocean and three poles, and the comparative study results between offshore and land, regional and global scientific issues.