Abstract：Hydrothermal sedimentary facies can be formed in rifted basins,mid-oceanic ridges,arc-basin system,as well as epeiric basins and intracontinental lacustrine basins. According to diagenetic and metallogenic modes,rock associations,and geochemical dynamic classifications,hydrothermal sedimentary lithofacies may be classified into hydrothermal syngenetic sedimentary lithofacies,hydrothermal quasi-syngenetic metasomatism lithofacies,hydrothermal syngenetic altered lithofacies,lithofacies of hydrothermal-blasting to hydraulic fracturing breccias,lithofacies of thermal brine quasi-syngenetic infiltration-metasomatism,and lithofacies of crytoexplosive to hydraulic fracturing breccias by hydrothermal fluids related to hydrothermal plume,including 17 types of tectonic lithofacies. All of them are of basic to establishment of independent tectonic mapping elements. The root,vent,center,proximate,and distal facies of the hrdrothermal fluid system have obvious tectonic lithofacies zonation and distribution in basins. However,all of them experienced deformations such as cataclastic rock facies,mylonite facies,and facies of the altered rocks related to thermal fluid reworking,overprinting,and reconstruction in intrcontinental orogens. After studies on deformation history and deformation-sieving of tectonic lithofacies,their tectono-palaeogeography units can be better understood. It may further help us to improve detecting buried tectonic lithofacies and mineral resource predication.
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