The Scientific Research Fund of the Second Institute of Oceanography under contract Nos JG2011 and JG1516;the National Natural Science Foundation of China under contract No.41606090;the National Basic Research Program(973 Program)of China under contract No.2015CB755904.
Sediment collapse and subsequent lateral downslope migration play important roles in shaping the habitats and regulating sedimentary organic carbon(SOC)cycling in hadal trenches.In this study,three sediment cores were...
funded by the National Key Research and Development Program of China(2016YFC0601005);the Geological Survey of China(DD20190370,DD20190811,cdcgs2018001);the National Science Foundation of China(41772107,41772016);the 13th Five-year Plan of the Ministry of Science and Technology of China(2016ZX05034-002-003)。
The continent of China developed through the coalescence of three major cratons(North China, Tarim and Yangtze) and continental micro-blocks through the processes of oceanic crust disappearance and acceretionary-colli...
Supported by the National Basic Research Program of China(973 Program)(No.2015CB755904);the National Natural Science Foundation of China(No.41676067);the Fundamental Funds for Central Universities,China(No.201762030);the Overseas Expertise Introduction Project for Discipline Innovation(111 Project)(No.B13030)。
Two sediment cores were retrieved in the hadal zone of the Yap Trench,and their concentrations of six major elements Mg,Al,Ca,Ti,Mn and Fe and nine trace elements Sr,Ba,Pb,V,Cr,Co,Ni,Cu and Zn were determined in induc...
funded by the National Natural Science Foundation of China (NSFC) (No. 41530966);Key Project of the Ministry of Science and Technology of China (No. 2016YFA0600904)
Diversion of the Yellow River is a unique geological event in offshore China,causing changes of the sedimentary environment in eastern China Seas.The last diversion took place in AD 1855,with the estuary diverted from...
supported by the National Basic Research Program of China (973 Program, No. 2014CB239001)
The Ordos Basin is the largest petroliferous basin in China, where the Chang 7 Member shale serves as the major source rock in the basin, with an area of more than 100,000 km^2 So far, sedimentary and geochemical char...
Supported by the National Key Basic Research and Development Program(973 Project);National Science and Technology Major Project(2016ZX05050,2017ZX05001002)
Paleo-sedimentary environment of Chang 7 Member of Upper Triassic Yanchang Formation in Ordos Basin, including the paleoclimate, paleo-salinity and paleo-redox conditions were restored through geochemical elements ana...
National Natural Science Foundation of China,No.41530962,No.41625021;The National Basic Research Program of China,No.2013CB956500;Natural Science Foundation of Jiangsu Province,No.BK20130056
Knowledge of the sediment flux derived from different sources is critical for interpreting the sedimentary records associated with large river sedimentary systems. For the Changjiang River system, previous studies har...
Supported by the National Basic Research Program of China(973 Program)(No.2012CB956004);the Fundamental Research Funds for the Central Universities(No.16lgjc22)
Coastal seas,located between continents and the open ocean,are an important active carbon pool.The sedimentary total organic carbon(TOC)in these areas is a mixture of terrestrial and marine sources,and can be a powerf...
supported by the Chinese National Key Project for Basic Research(grant No. 2011CB403007);the National Natural Science Foundation of China(grant No.41602127)
Objective The Simao Basin in Yunnan Province has developed Cretaceous evaporite-bearing clastic deposits, including the Mangang and Mengyejing Formations which were originally interpreted as fluvial and lacustrine dep...
supported by the National Basic Research Program of China (Grant Nos.2011CB403003 and 2013CB956403);"Strategic Priority Research Program" of the Chinese Academy of Sciences (Grant No.XDB03020402);the National Natural Science Foundation of China (Grant No.41272128);the College Research Program of Gansu Province (Grant No.2016A-123)
The Qiangtang Basin(QB), located in the central Tibetan Plateau, is a Jurassic marine basin and one of the most important prospective salt resource belts in China. In recent decades, many outcrops of gypsiferous bed...