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《Journal of Jiling University (Earth Science Edition)》 1991-01
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THE CEOLOGICAL AND GEOCHEMICAL CHARACTERICS OF CARBONATE IN EARLY PROTEROZOIC AULACOGEN IN LIAODONG

Wang Zhonghui(Bureau of Geology & Mineral Resources of Liaoning)Ma Qing(Geological Museum of China)  
The complex carbonate suite,appearing upset"S"shape, distributed along the trasition belt from miosyncline to eugeosync line in Liaodong early pro-terozoic aulacogen.It occure in transition belt environment that the basement is quite active in aulacogen. The lower part of the sequence is composed of Ca-carbonate,interbedded with basic volcanic rock.tuffaceous sediment rock, formed complex thin bedded structure.The middle part consist of thick,pure dolo-carbonate,there are several silicilith beds that formed by the exhalation on the ocean bottom in it,and a companied with sulphide mineralization. The upper part of the sequence is a thick Mg-carbonate and terminated at ma-gnesite to top of the suite. The REE features and Fe-Mn indices show that the carbonate have consistency with silicilith and sulphide, the results of lead isotope stand for that the origin is deep,and the carbon-oxygen isotope figure show that the carbonate have a special genesis.
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