supported by the National Science Foundation of China(No.41827802);performed at GeoSoilEnviroCARS(Sector 13-ID-D);Advanced Photon Source(APS),Argonne National Laboratory(ANL);supported by the National Science Foundation-Earth Sciences(No.EAR-1634415);the Department of Energy,Geosciences(No.DE-FG02-94ER14466);APS is supported by DOE-BES(No.DE-AC02-06CH11357).
The podiform chromitites in the Luobusha ophiolite have been thought to experience a very deep formation,but the maximum depth is still an open issue.Here,we have investigated the structural stability of natural magne...
supported by JSPS KAKENHI Grant Numbers 16H05741,19KK0092;Kana-zawa SAKIGAKE 2018 to T.M.,and 20 K14571 to H.S..K.S.thanks the Carlsberg Foundation for support via grant CF18-0090.
The Ujaragssuit Nunat layered(UNL)unit in the Itsaq Gneiss Complex,west Greenland,has been consid-ered to contain one of the oldest chromitites on Earth based on~ca.4.1 Ga Hadean whole rock Pt-Os model ages and ca.3.8...
the Research committee of Shiraz University and the Iranian Mineral Processing Research Center(IMPRC)that provided financial support for this study。
The Nain ophiolite complex with an extent of[600 km2 is a part of the Central Iranian ophiolite,which is related to the opening and subsequent closure of the Neo-Tethys Ocean.Dunite and serpentinized harzburgite in th...
supported by the National Natural Science Foundation of China (Grant Nos. 91755205, 41973012, and 41772055)。
Although the involvement of hydrous fluids has been widely invoked in formation of podiform chromitites in ophiolites, there is lack of natural evidence to signify the role and mechanism of fluids. In this study, a ne...
provided by the Fondo Europeo de Desarrollo Regional(FEDER)Funds;the Spanish Project CGL2015-65824 granted by the Spanish Ministerio de Economía y Competitividad(MINECO)to JAP and RTI2018-099157-A-I00 Ministerio de Ciencia;Innovacion y Universidades(MICINN)to JMGJ.Additional funding was obtained from the Ramon y Cajal Fellowship RYC-2015-17596 to JMGJ(sponsored by MICINN);the Ph.D.grant BES-2016-076887 to JFdP(sponsored by MINECO);the Mexican research programs Ciencia Basica(A1-S14574);sponsored by the Consejo Nacional de Ciencia y Tecnología(CONACYT)from Mexico,and the Programa de Apoyo a Proyectos de Investigacion e Innovacion tecnologica(IA-101419);sponsored by the UNAM.Additional support was provided by the University of Barcelona and University of Granada,Spain。
Chromitite bodies hosted in peridotites typical of suboceanic mantle(s.l.ophiolitic)are found in the northern and central part of the Loma Caribe peridotite,in the Cordillera Central of the Dominican Republic.These ch...
supported by the National Programme on Global Change and Air-Sea Interaction (No. GASI-GEOGE-02);the National Nature Science Foundation of China (Nos. 41772040,91858104);the Fundamental Research Funds for the Central Universities,Hohai University (No. 2013/B18020030)。
Reactions between a boninitic or basaltic magma and harzburgite at shallow mantle depths are thought to be closely related to the formation of podiform chromitites,but little experimental data is available on these re...
funded by grants from the International Geoscience Programme(IGCP 649,2015–2020);the Natural Science Foundation of China(41802055 and 41802034);the project from the China Postdoctoral Science Foundation(2018M632942);the Natural Science Foundation of Jiangsu(BK20180349);the Research Founding from Chinese Academy of Geological Sciences(J1903);the fund from the Key Laboratory of Deep-Earth Dynamics of Ministry of Natural Resources
Geophysical investigations and laboratory experiments show evidence for possible subduction of ancient oceanic crust.Geological and mineralogical observations suggest that subducted oceanic crust is recycled into the ...
granted by the Sultan Qaboos University Internal Grant(Grant No.IG/DVC/ESRC/18/01)
One of the major topics of debate in ophiolite geology is the original tectonic setting of ophiolites. New studies show that most ophiolites are formed more frequently in a suprasubduction zone(SSZ) environment and th...
Based on the textural and crystallographic study of four chromitite sites in the Oman ophiolite, we show that chromite crystallized in situ at Moho transition zone, where exposed as podiform chromitite deposits. Cryst...
granted by National Natural Science Foundation of China(Grant No.41720104009);China Geology Survey Project(Grant No.DD20160023-01);Foundation of MLR(Grant No.201511022)
The Dingqing ophiolite is located in the eastern segment of the Bangong-Nujiang suture zone. This suture zone is W–E trending parallel with the Yarlung–Zangbo suture zone and is an strategic area for exploring chrom...