Current Geological Issues and Future Perspectives in Deep-Time Source-to-Sink Systems of Continental Rift Basins  

作　　者：Qianghu Liu Zhiyao Li Hehe Chen Ziqiang Zhou Mingxuan Tan Xiaomin Zhu 

机构地区：[1]School of Earth Resources,China University of Geosciences,Wuhan 430074,China [2]School of Earth Sciences,Zhejiang University,Hangzhou 310058,China [3]School of Ocean Sciences,China University of Geosciences,Beijing 100083,China [4]School of Earth Science and Engineering,Imperial College London,London SW72AZ,United Kingdom [5]School of Ocean Sciences,Hohai University,Nanjing 210098,China [6]College of Geosciences,China University of Petroleum,Beijing 102249,China

出　　处：《Journal of Earth Science》2024年第5期1758-1764,共7页地球科学学刊（英文版）

基　　金：funded by the National Natural Science Foundation of China(Nos.41902112,42306083,42002117)。

摘　　要：0 INTRODUCTION Essentially,the source-to-sink systems are natural framework that follow the law of conservation of matter.The multifactor configuration link between provenance signals,geomorphological elements,and sedimentary records is mostly described in terms of weathering,denudation,transportation,and the accumulation of detrital particles(Helland-Hansen et al.,2016;Romans et al.,2016;Allen et al.,2013;Allen,2008a).

关 键 词：SEDIMENTARY mostly WEATHERING 

分 类 号：P512.2[天文地球—地质学] P531P539.2