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《Geotectonica Et Metallogenia》 2002-01
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EFFECT OF THE TAN -LU FAULT ON THE FORM ATION OF MINERAL DEPOSITS AND OIL-GAS FIELDS

HE Ying1 ,ZHANG Zhan-jun1,MAO Jing-wen 2 ,ZHANG Rong-hua2 (1.The Key Laboratory of Continental Dynamics,Ministry of Education;De partment of Geology,Northwest University,Xi 'an Shaanxi 710069,China;2.Institu te of Mineral Resources,Chinese Aca de  
The Tan -Lu fault is a multi-active fa ult zone,which may reach as deep as ma ntle.With the formation and evolution of the Tan -L u fault,different kinds of deposits and oil-gas fields have been formed.Since Palaeozoic Era,the character of the Tan -Lu fault zone changed from tension through compresso-shear to torsion-tension,the accompanying magmatism evolved from ultrabasic and basic through acidic to basic an d alkaline,and the related deposits a nd oil-gas fields revolved from magm atic deposits(such as diamond,Cr,Ni,Cu,Fe ect)through hydrothermal deposits(such as,Au,Mo,W,Sn,Pb,Zn,Hg,Sb,A g)and oil-gas fields to Au,Ag,gem deposit s and petrol,hydrocarbon,non-hydr ocarbon gas fields.The mineral-ization related to the Tan -Lu fault z one may be characterized by obvious s tages,symmetry-like,intersectin g and differences between the two sides of the fault zone,which may be contr olled by longitudinal-transversal features of the Tan -Lu fault,the nature of the massif which the Tan -Lu fau lt cuts through and the nature of the folds trending EW and crosscut ing by the Tan -Lu fault.With the evolution of the Tan -Lu fault and the crust-mantle interactions to di fferent extent,the mantle-derived fluids may have different contribut ions to the formation of the different kinds of deposits and oil-gas fields,and t he combined action of mantle-derived and the Earth's crust-derived fluids caused by int ense crust-mantle interactions may be essential condition for the formation of the concentrated hydrothermal deposits.
【Fund】: 国家973项目(G1999043211);; 国家自然科学基金项目(49972034)资助.
【CateGory Index】: P542
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