The amphibolites from the Mauranipur and Babina regions are located in the central part of the Bundelkhand Craton(BuC),northern India.During the geodynamic evolution of the BuC,these amphibolites underwent medium-grad...
Final support for this study was jointly provided by the National Natural Science Foundation of China (Grant Nos.41802056,41972058,42030307);the China Postdoctoral Science Foundation (Grant2018M633554);the MOST Special Fund from the State Key Laboratory of Continental Dynamics (Grant 201210133);Young Talent fund of University Association for Science and Technology in Shaanxi,China (Grant20200703);China Geological Survey (Grant DD20190376).
The North Qaidam orogenic belt(NQOB) is generally considered to be an early Paleozoic ultrahigh pressure metamorphic belt,but increasing reports of the Neoproterozoic magmatic and metamorphic events indicate that the ...
funding from the Department of Science and Technology, Government of India(India) under the DST INSPIRE Faculty Scheme (Grant:DST/INSPIRE/04/2014/000221)
Phase equilibria modelling coupled with U–Pb zircon and monazite ages of garnet–cordierite gneiss from Vallikodu Kottayam in the Kerala Khondalite Belt,southern India are presented here.The results suggest that the ...
Partial funding for this project was produced by a Grant-in-Aid for Scientific Research(B) from Japan Society for the Promotion of Science(JSPS) to Tsunogae(Nos.22403017,26302009 and 18H01300)
Madagascar,a major fragment of Gondwana,is mainly composed of Precambrian basenent rocks formed by Mesoarchean to Neoproterozoic tectono-thernial events and recording a Pan-African metamorphic overprint.The Ranotsara ...
financially supported by the National Natural Science Foundation of China (Nos. 41802070,41572051);the China Postdoctoral Science Foundation (No. 2018M631319);the Fund from the Key Laboratory of Deep-Earth Dynamics of Ministry of Natural Resources
Yushugou granulite-peridotite complex,located at the east part of the northern margin of South Tianshan,may represent an ophiolitic slice subducted to 40–50 km depth with high-pressure granulite facies metamorphism.A...
supported by the National Natural Science Foundation of China (No. 41872053);the NSF of Shandong Province (No. ZR2019BD046);the Chinese Ministry of Science and Technology (No. 2015CB856103);the Opening Foundation of the State Key Laboratory of Continental Dynamics, Northwest University (No. 17LCD07);SDUST Research Fund (No. 2015TDJH101)
The kyanite-bearing garnet pelitic gneiss from the Jianggalesavi area in southern Altyn Tagh high pressure/ultra-high pressure belt was proved to have been experienced UHP metamorphism (>12 GPa) by the discovery of ky...
the CARLSBERG FOUNDATION for support to carry out this work via grant CF16-0059
Corundum(ruby-sapphire) is known to have formed in situ within Archean metamorphic rocks at several localities in the North Atlantic Craton of Greenland. Here we present two case studies for such occurrences:(1) Manii...
financially supported by the National Natural Science Foundation of China(Grants 41330210,41520104004)
As a window of insight into the lower crust, high pressure granulite has received much attention since last decade. Yushugou high pressure granulite-peridotite Complex was located in the northeast margin of Southern T...
Pseudosection modelling is rapidly becoming an essential part of a petrologist's toolkit and often forms the basis of interpreting the tectonothermal evolution of a rock sample, outcrop, or geological region. Of the ...
financially supported by National Natural Science Foundation of China(Nos 41372004,41330210,41121062)
Metapelite is one of the predominant rock types in the high-pressure–ultrahigh-pressure(HP–UHP) metamorphic belt of western Tianshan, NW China; however, the spatial and temporal variations of this belt during meta...