T
Tang Hongfeng
Researcher at Chinese Academy of Sciences
Publications - 5
Citations - 20
Tang Hongfeng is an academic researcher from Chinese Academy of Sciences. The author has contributed to research in topics: Schist & Metamorphism. The author has an hindex of 3, co-authored 5 publications receiving 19 citations.
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Journal Article
Trace Element Geochemistry of A-Type Granites
TL;DR: In this article, a comparison of trace element geochemical characteristics of A-type granites and those of the associated aluminous granites in several areas is presented. And the results show that the alkaline A type granites have higher Ga and F concentrations, smaller LREE/HREE ratios, lower Eu, Ba, etc.
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Elemental geochemistry and Nd isotopic characteristics of the metasedimentary rocks from the metamorphic belt in central Jiangxi: Provenance and tectonically environmental constraints
TL;DR: The metamorphic belt in central Jiangxi, located in the compound terrain within the Cathaysia, Yangtze Block and Caledonian fold zone of South China, is composed dominantly of meta-argillo-are-naceous rocks, with minor amphibolite.
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Reaction experiments between tonalitic melt and mantle olivine and their implications for genesis of high-Mg andesites within cratons
Wang Ming-Liang,Tang Hongfeng +1 more
TL;DR: This article performed reaction experiments between tonalitic melt and mantle olivine on a six-anvil apparatus at high-temperature of 1250-1400°C and high-pressure of 2.0-5.0 GPa.
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Rb-Sr isotopic chronology of the Au-bearing quartz veins in gold deposits in the eastern part of north China platform
TL;DR: In this paper, the authors have selected some isotope data (including four gold deposits previously studied and two gold deposits in this work ) of Au-bearing quartz veins of the representative gold deposits and calculated their metallogenic ages using the method of Ludwig.
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The Elastic Wave Velocities of the Granitoids from Eastern Junggar of Xinjiang at High Temperature and High Pressure and Their Geological Constraints on the Crustal Structure
TL;DR: In this paper, the authors measured the compressional and shear wave velocities of typical granitoids (alkali-feldspar granite, alkaline granite, granodiorite, monzogranite and quartz diorite) from Kalamaili granite belt and Yemaquan body in Eastern Junggar, Xinjiang were experimentally measured at pressures up to 1.0 GPa (room temperature) and temperatures up to 700°C by ultrasonic reflection-transmission method.