A5112498647- Geological and Geochemical Analysis
- earthquake and tectonic studies
- High-pressure geophysics and materials
- Geochemistry and Geologic Mapping
- Geochemistry and Geochronology of Asian Mineral Deposits
- Geological and Geophysical Studies
- Geochemistry and Elemental Analysis
- Paleontology and Stratigraphy of Fossils
- Hydrocarbon exploration and reservoir analysis
- Geological Studies and Exploration
- Geoscience and Mining Technology
- Atmospheric and Environmental Gas Dynamics
- Methane Hydrates and Related Phenomena
- Geology and Paleoclimatology Research
- Geomechanics and Mining Engineering
- Glass properties and applications
- Mycorrhizal Fungi and Plant Interactions
- Mining and Resource Management
- South Asian Studies and Conflicts
- Fungal Biology and Applications
- Geotechnical and Geomechanical Engineering
- Forest Insect Ecology and Management
- Cultural Heritage Materials Analysis
- Military History and Strategy
- Geological and Tectonic Studies in Latin America
China University of Geosciences (Beijing)
2015-2024
China University of Geosciences
2000-2015
State Key Laboratory of Geological Processes and Mineral Resources
2013-2015
Beijing Institute of Geology for Mineral Resources
2013
Ministry of Education of the People's Republic of China
2004
New geochronological and geochemical data on magmatic activity from the India-Asia collision zone enables recognition of a distinct flare-up event that we ascribe to slab breakoff. This tie-point in collisional record can be used back-date time initial impingement Indian continent with Asian margin. Continental arc magmatism southern Tibet during 80-40 Ma migrated south north then back significant mantle input at 70-43 Ma. A pronounced flare up intensity (including ignimbrite mafic rock) ca....
Generation of continental crust in collision zones reflect the interplay between oceanic subduction and collision. The Gangdese southern Tibet developed during Neo-Tethyan slab Mesozoic prior to reworking India-Asia Cenozoic. Here we show that arc magmatism started with fractional crystallization form cumulates associated medium-K calc-alkaline suites. This was followed by a period commencing at ~70 Ma dominated remelting pre-existing lower crust, producing more potassic compositions....
The continental crust in the overriding plate of India-Asia collision zone southern Tibet is characterized by an overthickened layer felsic composition with underlying granulite-eclogite layer. A large data set indicates that this experienced magmatism from 245 to 10 Ma, as recorded Gangdese Batholith. Magmatism was punctuated flare-ups at 185−170, 90−75, and 55−45 Ma caused a combination external internal factors. growth starts period dominated fractional crystallization formation...
Research Article| July 01, 2009 The 132 Ma Comei-Bunbury large igneous province: Remnants identified in present-day southeastern Tibet and southwestern Australia Di-Cheng Zhu; Zhu * 1State Key Laboratory of Geological Processes Mineral Resources, China University Geosciences, Beijing 100083, *E-mail: dchengzhu@163.com; moxx38@yahoo.com. Search for other works by this author on: GSW Google Scholar Sun-Lin Chung; Chung 2Department National Taiwan University, Taipei 106, Xuan-Xue Mo; Mo Zhi-Dan...
Research Article| July 01, 2010 Presence of Permian extension- and arc-type magmatism in southern Tibet: Paleogeographic implications Di-Cheng Zhu; Zhu † 1State Key Laboratory Geological Processes Mineral Resources, School Earth Science China University Geosciences, Beijing 100083, †E-mail: dchengzhu@163.com Search for other works by this author on: GSW Google Scholar Xuan-Xue Mo; Mo Zhi-Dan Zhao; Zhao Yaoling Niu; Niu 2Department Sciences, Durham University, DH1 3LE, UK Li-Quan Wang; Wang...