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(古)岩溶与成矿,国内外正大力研究,并发现很多矿产资源,如铅、锌、钢、钠、金等,与(古)岩溶作用有关。这不仅在找矿上取得了新的突破,同时促进了成矿理论的发展。我国地质构造复杂,尤其进入地洼活动阶段,地壳运动强烈,地貌反差大,(古)岩溶发育,寻找(古)岩溶矿床有着广阔的前景。(古)岩溶矿床的含矿主岩,是(古)岩溶堆积岩。这类岩石具有独特的结构和构造。在几何形态上呈礁状、柱状、脉状、管状和槽状的地质体。发育和保存于地史上断陷或拗陷带,并以后接受沉积的低缓区。如中生代和第三纪
(Paleo) karstification and mineralization are being studied both at home and abroad, and many mineral resources such as lead, zinc, steel, sodium and gold are found, which are related to (karstified) karstification. This not only made new breakthroughs in prospecting, but also promoted the development of metallogenic theory. The geological structure of our country is complex, especially in the active stage of Diwa, with strong crustal movement, large contrast in landscape, (karst) karst development and the search for (ancient) karst deposits. (Ancient) karst ore-bearing host rocks, is (ancient) karst accumulation rock. These rocks have unique structures and structures. Geometrically reef-shaped, columnar, vein-shaped, tubular and trough-shaped geological body. Developed and preserved in the history of depression or depression zone, and later accepted the deposition of slow zone. Such as Mesozoic and Tertiary