中文摘要：

为了进一步查明内蒙古东乌珠穆沁旗朝不楞矽卡岩型铁多金属矿床的形成时间，对主要铁多金属矿体4件辉钼矿样品进行了铼-锇同位素分析，所获同位素等时线年龄为（140．7±1．8）Ma（2α），其MSWD值为1．12。鉴于辉钼矿呈稀疏浸染状和条带状分布在铁多金属矿石中，并且与磁黄铁矿和黄铜矿呈共生结构关系，可以推测朝不楞铁多金属矿床的形成时间为早白垩纪，属燕山期构造一岩浆活动的产物。朝不楞矽卡岩型铁多金属矿床形成时代的厘定对于提高该矿床的理论研究水平和指导隐伏金属矿床的找矿勘查工作均具有重要意义。

英文摘要：

Located in the easternmost part of the Chaganobo-Aoyoute-Chaobuleng Early Paleozoic tectono-magmatic belt on the southern edge of the Siberian plate, the Chaobuleng deposit is a medium-size skarn iron-polymetallic deposit occurring in central-eastern Inner Mongolia. Systematic drilling results show that the deposit contains metal reserves of Fe 1.9 Mt, Bi 17xl04 t, Ag222 t, Sn0.61 xl04 t, Cu3.06xl04 t, Au 1.68 t, Pb9518 tandW3979 t. The unique geology of the deposit has attracted the attention of ore geologists from China and abroad. During the Mesozoic Yanshanian orogeny, inten- sive tectonic and igneous activities resulted in the large-scale granitoid plutonism and relevant contact metasomatism in Chaobuleng and its neighboring areas. The Chaobuleng gabbro and granitoid stocks were emplaced in the Middle Devonian sedimentary sequence of the Taerbagete Group, controlled by the NE-trending fault zone. A large number of skarn blocks are located along the contact zone between these two intrusive stocks and their carbonate wall rocks. Although the gabbro and granite stocks show obvious differences in textures and mineral assemblages, both of them belong to alkaline-rich calc- alkaline igneous series. Iron-polymetallic mineralization occurs exclusively along the contact zone between the Mesozoic intrusive stocks and the Middle Devonian sedimentary sequences in the forms of pillars, cylinders, stratoid lenses and lay- ers. The main metallic minerals of the iron-polymetallic ore from Chaobuleng are magnetite, pyrite, chalcopyrite, molybde- nite, sphalerite, pyrrhotite, scheelite, galena, arsenopyrite, marcasite, bornite, bismutinite, galenobismutite, and native bismuth. The gangue mineral assemblage consists mainly of diopside, amphibole, grossular, andradite, almandine, vesuvi- anite, tremolite, actinolite, plagioclase, epidote, quartz, biotite, sericite, chlorite and calcite. Re-Os isotopic age dating of four molybdenite separates from the No. I mineralized zone gives an isochron age of （ 140.7 ＋ 1.8 ） Ma, and