GEOCHEMICAL CRITERIA FOR URANIUM METALLOGENE-TIC CAPACITY OF GRANITOIDS IN SOUTH CHINA--《Chinese Journal of Nuclear Science and Engineering》1988年02期
GEOCHEMICAL CRITERIA FOR URANIUM METALLOGENE-TIC CAPACITY OF GRANITOIDS IN SOUTH CHINA
ZHANG BANGTONG DAI YONGSHAN WANG NIANSHENG LIU JISHUN (Department of Geoscience, Nanjing University)
Based on research of uranium distribution for 11 uranium-bearing granitic, plutons in South China, come to some geochemical criteria, favorable to form granite-type uranium deposits, as follows: the average uranium content of uranium-hearing granites in South China is 9.94 ppm (for 906 samples), being 2.84 times higher than that of the granite rocks of the whole world (3.5ppm); the coefficient of variation of uranium contents in uranium-bearing granites is high (350%) and the frequence distribution curves of U the factor (K_f) of crystalline concentration of U for host rock is greater than 1.5; the existence of "Th/U turn" in the uranium-bearing multistaged composite granite of transformation type i the nonstructure uranium in the uranium ore-forming host rocks exceeds 15% of total uranium content.
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(C)2006 Tsinghua Tongfang Knowledge Network Technology Co., Ltd.(Beijing)(TTKN) All rights reservedGENESIS OF RAPAKIVI FELDSPAR AND DARK-COLOURED ENCLAVES OF THE YAOCUN GRANITE BODY IN SOUTHERN ANHUI--《Geological Review》1990年01期
GENESIS OF RAPAKIVI FELDSPAR AND DARK-COLOURED ENCLAVES OF THE YAOCUN GRANITE BODY IN SOUTHERN ANHUI
Ling Hongfei, Zhai Jianping and Zhang Bangtong (Earth Science Department, Nanjing University)
The Yaocun granite body is characterized by a lot of dark-coloured enclaves and rapakivi feldspars. It was discovered that there is close relationship between them. there are no rapakivi feldspars in the granite unless the appearanee of dark-coloured enclaves. In dark-coloured enclaves there are often rapakivi ieldspar whose characters are the same as those of rapakivi fe for example, their cores (perthite) have Carlsbad twins and resorbed outlines, the contents and changing trend of the major elements and barium are similar, The dark enclaves are fine-grained quartz-hornblende monzonite with typical igneous textures such as girdles and resorption of hornblende and plagioclase and poikilitic texture. This suggests a magmatic genesis for the enclaves, Further research came to the conclusion that dark enclaves were formed by incomplete mixing of intermediate-basic magma with granitic magma. The chief evidence is as follows: fluidal structure and fine-grained rims along the contact of enclaves with granite, existence of acicular apatite in enclaves, and presence of broken rapakivi feldspar whose cracks are infilled with minerals of host rocks. This implies that K-feldspar in enclaves crystallized in granitic magma and migrated into intermediate-basic magmatic balls trapped by the granitic magma, thus forming rapakivi feldspar, As granite magma was contaminated by intermediate-basic magmas, the Ca content increased locally and K-feldspar ceased to grow. whereas plagioclase crystal- lized by means of selecting K-feldspar with lattice similar to that of plagioclase as the growth base, thus forming rims of plagioclase. Afterwards such mush magma was further emplaced to a higher level and crystallized rapidly, thus forming relatively fine-grained matrix.
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(C)2006 Tsinghua Tongfang Knowledge Network Technology Co., Ltd.(Beijing)(TTKN) All rights reservedNeodymium Isotope Composition and Source Materials of the Meta-basement in Central Jiangxi Province--《ACTA PETRROLOGICA ET MINERALOGICA》1998年01期
Neodymium Isotope Composition and Source Materials of the Meta-basement in Central Jiangxi Province
Hu Gongren, Zhang Bangtong
(Department of Earth Sciences, Nanjing University, Nanjing
In this paper, the neodymium isotope composition and source materials of the meta-basement in central Jiangxi have been studied. The Presinian medium-grade metamorphosed sedimentary rocks have lower
Nd ratio (0..512052) and ∈
) values (-3.60—+1.11) and older model ages ( Ma), while the slightly metamorphosed Sinian sedimentary rocks have a bit higher
Nd ratios (0..512233) and ∈
) values (-0.320—-0.55) and younger model ages ( Ma). The above neodymium isotope characteristics suggest that the Presinian metamorphic sedimentary rocks consist of old continental debris from Huaxia massif and volcanic materials derived from the mantle, being formed in an arc-type environment. The Sinian epimetamorphic sedimentary rocks were formed along the western active margin of Huaxia paleocontinent, with their rock-forming materials derived chiefly from eroded debris of Presinian metamorphic sedimentary rocks and a bit volcanic materials. The above study has provided important isotopic evidence for the argument that meta-basement in central Jiangxi belongs to Huaxia massif.
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