financially supported by the National Natural Science Foundation of China(Grant Nos.41671011,41871019,41877292,41972212);Research Foundation of Chutian Scholars Program of Hubei Province(Grant No.8210403);Shanxi Key Research and Development program:Feng Cheng(Grant No.2021SF2-03).
Plate subduction leads to complex exhumation processes on continents.The Huangling Massif lies at the northern margin of the South China Block.Whether the Huangling Massif was exhumed as a watershed of the middle reac...
Introduction to the Middle-Lower Yangtze River Valley Metallogenic Belt The Middle-Lower Yangtze River Valley metallogenic belt(MLYB)has been a cradle of modern metallogeny in China.In the MLYB,there are numerous stra...
supported by the National Science Foundation of China(41925011);the National Key Research and Development Program of China(2016YFC0600206);China University of Geosciences(3-8-2020-002);China Geological Survey(DD20201173);Hubei Sanxin Gold Copper Limited Company(CG-2019-HX-S004)。
Cu and Fe skarns are the world's most abundant and largest skarn type deposits,especially in China,and Au-rich skarn deposits have received much attention in the past two decades and yet there are few papers focused o...
funded by grants from the National Key Research and Development Program(2016YFC0600206);the National Natural Science Foundation of China(41872081);the Doctoral initial funding project of Anhui Jianzhu University(2019QDZ33);the Anhui Province Science and Technology Plan Project for Housing Urban-rural Construction(2020-YF35)。
The Middle-Lower Yangtze River Metallogenic Belt(MLYB)is known to contain abundant copper and iron porphyry-skarn deposits,with an increasing number of tungsten deposits and scheelite in Fe-Cu deposits being discovere...
supported by the National Key R&D Program of China(No.2016YFC0600404);the National Natural Science Foundation of China(Grant Nos.41673040 and 41611540339);the Project of National Land Resource Science and Technology of Anhui Province(2014-K-4)
The newly discovered Paodaoling porphyry Au deposit from the Guichi region, Lower Yangtze River Metallogenic Belt (LYRB), contains 〉35 tons of Au at an average grade of -1.7 g/t. It is a porphyry 'Au-only' deposi...
supported by the National Science Foundation of China(grants No.41372090 and 41573042);the National Special Research Programs for Non-Profit Trades (grant No.201311136);Basic Scientific Research Operation Cost of State-Leveled Public Welfare Scientific Research Courtyard(grant No.K1203)
Thallium has been used geochemical exploration of gold deposits. However, as an indicator element in searching for hydrothermal the T1 minerals and mineralization are rare in nature. Lorandite T1AsS2, a relatively un...
financially supported by the National Natural Science Foundation of China (grants No.41072083 and 4157209)
Objective In recent years, the birth time and evolution of the Three Gorges, Yangtze River has become a focused topic. Different from previous studies, this study used provenance analysis of Quaternary sediments to di...
supported by geological survey projects of the China Geological Survey (1212011120863, 12120114039401, 12120114005901 and 12120115029401)
The Tongshankou Cu-Mo deposit, located in southeast Hubei province, is a typical skarn–porphyry type ore deposit closely related to the Tongshankou granodiorite porphyry, characterized by a high Sr/Y ratio.Detailed i...
supported by the National Natural Science Foundation of China (Item No. 40673005);the Ministry of Science and Technology (2004DIB3J081);the Geological Survey of China (200320130-006)
The chemical and isotopic characteristics of the water and suspended particulate materials(SPM) in the Yangtze River were investigated on the samples collected from 25 hydrological monitoring stations in the mainste...
supported by the National Natural Science Foundation of China (Grant No. 40930419);the National Special Research Programs for Non-Profit Trades (Sponsored by MLR, Grant Nos. 200911007 and 200811114);Open Foundation of State Key laboratory of Geological Processes and Mineral Resources, School of the Earth Sciences and Resources, China University of Geosciences, Beijing (Grant No. GPMR201029)
Late Mesozoic volcanic-subvolcanic rocks and related iron deposits, known as porphyry iron deposits in China, are widespread in the Ningwu ore district (Cretaceous basin) of the middle-lower Yangtze River polymetall...