supported by the National Natural Science Foundation of China(Grant Nos.42072058,41772054,41572039)。
Monazite is an important accessory mineral in the pelitic granulites(Weihai area,Sulu orogen),and is also a powerful monitor for understanding the metamorphic evolution of the granulites.The pelitic granulites incongr...
supported by the National Natural Sciences Foundation of China(Grants Nos.41172189,40972137,and 41402179)
Suizhou-Zaoyang area is located in the southern Qinling-Tongbai-Dabie Orogen, China. A combined research on U-Pb ages and Lu-Hf isotopes for detrital zircons from three meta-sedimentary rocks in the Wudang Group is re...
supported by the Major State Basic Research Programme of the People’s Republic of China(Grant No.2012CB416601);the Knowledge Innovation Programme of the Chinese Academy of Sciences(Grant No.KZCX2-YW-Q04-07)
In China, most Precambrian banded iron formations (BIFs) are situated in the North China Craton. The Yuanjiacun iron depos- it, located in the Ltlliang area, is arguably the most representative Superior-type BIF. Th...
supported by National Natural Science Foundation of China (Grant No.41002062);Scientific Research Program of the Ministry of Science and Technology of China (Grant No. J0901);the Key Program of the Land and Resource Ministry of China (Grant Nos. 1212011120151,1212010811033, 1212010711815)
The Daqing Mountains area comprises a typical occurrence of the Khondalite Belt in the Western Block of the North China Craton (NCC). In this area, both early and late Paleoproterozoic metasedimentary rocks have been ...
supported by China Geological Survey (Grant Nos. 1212010611802,1212010711815 and 1212011120152);National Natural Science Foundation of China (Grant No. 41172171);Basic Foundation of Scientific Research Work from Ministry of Science and Technology of China (GrantNos. J0721 and J0907);National Commission on Stratigraphy of China(Grant Nos. 1212010511702-01 and 1212011120142)
Zircon U-Pb ages(SHRIMP and LA-ICPMS) and Lu-Hf isotope data(LA-ICPMS) are presented for two granite and two quartzite pebbles from the basal conglomerates of the Sijizhuang Formation in the Hutuo Group from the Wutai...
supported by National Natural Science Foundation of China (Grant Nos. 40730315 and 41023009);State Key Laboratory of Lithospheric Evolution
Hyalophane-rich pegmatites are identified from the Manjinggou high-pressure granulite terrain in the Central Zone of North China Craton. Based on field investigation, mineral assemblage and mineral geochemistry, two t...
Supported by National Natural Science Foundation of China (Grant No. 40634023)
A garnet-pyroxene bearing amphibolite as a xenolith hosted by the Mesozoic igneous rocks from Xuzhou-Suzhou area was dated by zircon SHRIMP U-Pb method, which yields a metamorphic age of 1918 ± 56 Ma. In addition, th...
the National Natural Science Foundation of China (Grant No. 40572113);China Geological Survey Important Base Research (Grant No. 2005CCV05600);1:250000 Geology Survey (Grant No. 20001300009231)
Granitic gneisses have been widely found in crystalline rocks in the Dinggye area of the Higher Himalaya (HHM) and the LhagoiKangri area of the North Himalaya (NHM), Tibet. In the HHM, the gneisses intruded in the gra...
This work was supported by an RGC Grant of Hong Kong,China(Grant Nos.HKU7115/00P and HKU7090/01P)
The basement of the North China Craton can be divided into the Eastern and Western Blocks and the Central Zone (Trans-North China Orogen). The West Block formed by the amal-gamation of the Ordos Block in the south and...
the National Natural Science Foundation of China (Grant Nos. 49972064, 49832030, 49929301).
Zircon U-Pb ages are reported for three samples of intrusive rocks in Khondalite series in the Sanggan area, North China craton. The age of meta-granite is dated as 2005±9 Ma, implying that the sedimentary sequences ...