华南地区中生代以来岩石圈伸展及其与铀成矿关系研究的若干问题
Some problems concerning relationship between Mesozoic-Cenozoic lithospheric extension and uranium metallogenesis in South China
查看参考文献123篇
|
文摘
|
华南地区中生代以来存在大规模的岩石圈伸展作用,与伸展作用相对应,形成了大量花岗岩型、火山岩型和碳硅泥岩型铀矿床。文章详细总结了华南中生代以来岩石圈伸展作用和铀成矿作用的研究进展。通过系统分析,认为要深刻揭示岩石圈伸展与区域铀成矿的关系,至少尚有两大重要科学问题未解决：其一是华南白垩纪—第三纪岩石圈伸展和铀成矿的准确期次及其空间迁移规律;其二为岩石圈伸展期铀成矿的必然性或铀为什么会集中在岩石圈伸展期成矿。要解决第一个问题,需要对铀矿床和岩石圈伸展期形成的基性脉岩开展系统的高精度定年工作;要解决第二个问题,则需要系统研究成矿流体中CO_2等气体组分在铀成矿中的作用及其成因。 |
|
其他语种文摘
|
Previous studies have shown that there existed large-scale lithospheric extension events during the Cretaceous-Tertiary period in South China, and that large-scale uranium mineralization occurred at the same time in this area, which resulted in the formation of many important uranium deposits such as granite-hosted, volcanicshosted and Carbonaceous-siliceous-pelitic sedimentary rock-hosted ones. This paper reviews previous researches on lithospheric extension and uranium metallogenesis in South China since Mesozoic, and preliminarily discusses their temporal and spatial associations. In order to precisely reveal the relationship between lithospheric extension and uranium metallogenesis, it is suggested that at least two fundamental problems should be solved. The first is the accurate episodes of extension and uranium mineralization, and the second is the mechanism governing the control of the tectonic regime over the formation of the uranium deposits. To probe into these problems, it is necessary to accurately date the uranium deposits and the magic dikes intruded during the Mesozoic extension and to determine the role and origin of gaseous components such as CO_2 in ore-forming fluids.
|
|
来源
|
矿床地质
,2007,26(2):139-152 【核心库】
|
|
关键词
|
地质学
;
白垩纪-第三纪
;
岩石圈伸展
;
幔源CO_2
;
铀成矿
;
华南
|
|
地址
|
中国科学院地球化学研究所, 矿床地球化学国家重点实验室, 贵州, 贵阳, 550002
|
|
语种
|
中文 |
|
文献类型
|
研究性论文 |
|
ISSN
|
0258-7106 |
|
学科
|
地质学 |
|
基金
|
国家自然科学基金重点项目
;
国家自然科学基金
;
中国科学院知识创新工程重要方向项目
|
|
文献收藏号
|
CSCD:2857831
|
参考文献 共
123
共7页
|
|
1.
Black L P. The difficulties of dating mafic dykes:an Antarctic example.
Contribution to Mineralogy and Petrology,1991,109:183-194
|
被引
10
次
|
|
|
|
|
2.
Bohlke J K. Laser microprobe analysis of noble gas isotopes and halogens in fluid inclusions-analysis of microstandards and synthetic inclusions in quartz.
Geochim. Cosmochim. Acta,1992,56:187-201
|
被引
5
次
|
|
|
|
|
3.
Burgess R. He, Ar, and C isotopes in coated and polycrystalline diamonds.
Chemical Geology,1998,146:205-217
|
被引
5
次
|
|
|
|
|
4.
Burgess R. Constrains on the age and halogen composition of mantle fluids in Siberian coated diamonds.
Earth Planet Sci. Lett,2002,197:193-203
|
被引
1
次
|
|
|
|
|
5.
Burgess R. Noble gas and halogen composition of mantle fluids in Canadian diamonds.
Geochim. Cosmochim. Acta,2004,68(11):A277-A277
|
被引
1
次
|
|
|
|
|
6.
Burnard P G. Importance of mantle derived fluids during granite associated hydrothermal circulation:He and Ar isotopes of ore minerals from Panasqueira.
Geochim. Cosmochim. Acta,2004,68:1607-1615
|
被引
31
次
|
|
|
|
|
7.
Burnard P G. Mantle, crustal and atmospheric noble gases in Ailaoshan gold deposits, Yunnan province, China.
Geochim. Cosmochim. Acta,1999,63:1595-1604
|
被引
116
次
|
|
|
|
|
8.
Campbell S D G. Structural control and tectonic setting of Mesozoic volcanism in Hong Kong.
Journal of the Geological Society of London,1997,154:1039-1052
|
被引
13
次
|
|
|
|
|
9.
Faure M. Doming in the southern foreland of the Dabieshan(Yangtze block, China).
Terra Nova,1998,18:307-311
|
被引
12
次
|
|
|
|
|
10.
Gilder S A. Timing and spatial distribution of rifting in China.
Tectonophysics,1991,197:225-243
|
被引
122
次
|
|
|
|
|
11.
Irwin J J. Diverse origins of fluid in magmatic inclusions at Bingham(Utah, USA), Butte(Montana, USA), St-Austell(Cornwall, UK), and Ascension-Island(Mid-Atlantic, UK), indicated by laser microprobe analysis of Cl, K, Br, I, Ba plus Te, U, Ar, and Xe.
Geochim. Cosmochim. Acta,1995,59:295-312
|
被引
4
次
|
|
|
|
|
12.
Kendrick M A. Noble gas and halogen evidence for the origin of Scandinavian sandstone-hosted Pb-Zn deposits.
Geochim. Cosmochim. Acta,2005,69:109-129
|
被引
7
次
|
|
|
|
|
13.
Kendrick M A. Fluid inclusion noble gas and halogen evidence on the origin of Cu-porphyry mineralizing fluids.
Geochim. Cosmochim. Acta,2001,65:2651-2668
|
被引
63
次
|
|
|
|
|
14.
Lee J. Ductile strain and metamorphism in an extensional tectonic setting:A case study from the northern Snake Range, Nevada, USA.
Geol. Soc. Spec. Publ.,1987,28:267-298
|
被引
1
次
|
|
|
|
|
15.
Leroy J. The Margnac and Fanay uranium deposits of the La Crouzille district(western Massif Central, France):Geologic and fluid inclusion studies.
Econ. Geol.,1978,73:1611-1634
|
被引
15
次
|
|
|
|
|
16.
Lister G S. The origin of metamorphic core complexes and detachment faults formed during tertiary continental extension in the northern Colorado River region, USA.
Journal of Structure Geology,1989,11:65-94
|
被引
85
次
|
|
|
|
|
17.
Malavieille J. Kinematics of compressional and extensional ductile shearing deformation in a metamorphic core complex of the northeastern Basin and Range NW.
Journal of Structure Geology,1987,9:541-554
|
被引
1
次
|
|
|
|
|
18.
Marignac C. Ore deposits of the French Massif Central:Insight into the metallogenesis of the Variscan belt.
Mineralium Deposita,1999,34:472-504
|
被引
20
次
|
|
|
|
|
19.
Marty B. Helium isotope and CO_2 in volcanic gases of Japan.
Chemical Geology,1989,76:25-40
|
被引
31
次
|
|
|
|
|
20.
Min M. Carbonaceous-siliceous-pelitic rock type uranium deposits in southern China:Geologic setting and metallogeny.
Ore Geology Reviews,1995,10:51-64
|
被引
4
次
|
|
|
|
|
了解气象卫星更多信息，请访问