supported by the National Natural Science Foundation of China(Grant No.41973045);Basic Science and Technology Research Funding of the CAGS(Grant No.JKYZD202312);the National Key Research and Development Project of China(Grant No.2022YFF0800903);National Natural Science Foundation of China(Grant Nos.41802113,42073053,42273073 and 42261144669).
Lamprophyres typically appear in hydrothermal gold deposits.The relationship between lamprophyres and gold deposits is investigated widely.Some researchers suggest that the emplacement of lamprophyres triggers gold mi...
The lamprophyres are late dykes that cut the formations hosting the gold mineralization in the Nassara deposit. They are geographically and spatially related to most orogenic gold deposits. It is with the aim of chara...
supported by the National Natural Science Foundation of China (Grant Nos. 91962105, 41802113);the Fundamental Research Funds for the Central Universities (Grant No.2019B08214);a grant from Jiangsu Provincial “Double Innovation Doctors” Program (Grant No.(2020) 30462)。
The xenoliths in host rocks of hydrothermal gold deposits can generally provide much geochemical information of the deep rocks, which may have an implication for the sources of ore-forming materials. Geochronology and...
the National Natural Science Foundation of China and Shandong Province(Nos.ZR2018BD019,41572182,41803031,41272225);the MOST Special Fund from the State Key Laboratory of Geological Processes and Mineral Resources,China University of Geosciences(Wuhan)(No.MSFGPMR02-3);the Youth Innovation Team Development Plan of the Universities in Shandong Province。
Lamprophyre dykes that crosscut different types of ultrahigh pressure(UHP)metamorphic rocks are widely distributed in the Triassic Sulu UHP orogenic belt.Although abundant studies have been performed on these dykes,th...
Detailed mineralogy,bulk rock major,trace and Sr-Nd isotope compositions,and ^(40)Ar/^(39)Ar dating of the Pipe-8 diamondiferous ultramafic intrusion in the Wajrakarur cluster of southern India,is reported.Based on th...
Mineralogical,geochemical and isotopic(Sr and Nd) studies on the recently reported ca. 124 Ma'anorogenic lamproite' dyke from the Palanpur area, Kutch seismogenic rift zone, northwestern India, are presented. We propo...
The various parts of Cudappah Igneous Provice(CIP)/Prakasham Alkaline Province(PAP)of the Eastern Dharwar Craton(EDC),southern India is known for the occurrence of lamprophyre.Present paper reports a
supported by the Seluk University Scientific Research Projects Coordination (Project No:11201041)
In the vicinity of Konya (Turkey),mafic,micro-porphyritic sub-volcanic rocks intrude into the Mesozoic units,which represents the only example of such a rock type in the region.40Ar/39Ar dating of two whole rock sam...
In the Abu Rusheid area, Southeastern Desert of Egypt, polymineralized (HREEs, U, Zn and Pb) lam-prophyre dykes are recently recorded. The lamprophyre dykes cut cataclastic rocks along share zones in NNW-SSE trends. T...
The Wadi Sikait area lies at about 95 km southwest of Marsa Alam City along the Red Sea Coast, Eastern Desert, Egypt. It is occupied by Precambrian rocks of ophiolitic mélange, metamorphosed sandstones (MSS), gab-bro...