CAJ | 학술논문

云南省武定县迤纳厂铁铜矿区广泛出露元古宙辉绿岩体。前人对区内基性岩浆岩研究程度较低，缺乏辉绿岩的形成时代资料。本文报道了区内海孜辉绿岩中锆石的LA-ICP-MS U-Pb年龄，为1728±4 Ma。此年龄与古元古代晚期扬子地台西南缘大规模非造山型岩浆活动及全球性 Columbia 超级大陆裂解时代高度一致，表明其可能为 Columbia 超级大陆裂解的产物。辉绿岩与区内铁铜矿床成矿时代大致相当，反映了古元古代晚期扬子地台西南缘大规模的岩浆活动也可能是一次重要的成矿事件，可能为铁、铜成矿作用提供主要的成矿物质来源。武定地区被辉绿岩侵入接触的原“美党组”地层的沉积时代应大于辉绿岩的侵位时代，应划入下元古界汤丹群，是昆阳陆内裂谷拉张以前就已存在的基底地层。
운남성무정현이납엄철동광구엄범출로원고주휘록암체。전인대구내기성암장암연구정도교저，결핍휘록암적형성시대자료。본문보도료구내해자휘록암중고석적LA-ICP-MS U-Pb년령，위1728±4 Ma。차년령여고원고대만기양자지태서남연대규모비조산형암장활동급전구성 Columbia 초급대륙렬해시대고도일치，표명기가능위 Columbia 초급대륙렬해적산물。휘록암여구내철동광상성광시대대치상당，반영료고원고대만기양자지태서남연대규모적암장활동야가능시일차중요적성광사건，가능위철、동성광작용제공주요적성광물질래원。무정지구피휘록암침입접촉적원“미당조”지층적침적시대응대우휘록암적침위시대，응화입하원고계탕단군，시곤양륙내렬곡랍장이전취이존재적기저지층。
There exists a large number of diabase rock bodies at the Yinachang iron-copper deposit in Wuding, central Yunnan Province, southwest China. So far, few research works have been carried out on the mafic rocks within this ore district, thus the age of the diabases remains poorly understood. In this paper, we report the zircon U-Pb age of the Haizi diabase obtained by LA-ICP-MS method, and the weighted mean 206Pb/238U age is 1728±4 Ma (MSWD=1.8, n=11). The age of the diabase in the Wuding area is consistent with the contemporary magmatism in the southwestern Yangtze Block, as well as the breakup of the Columbia supercontinent. Therefore, it is suggested that these diabases formed in response to the global breakup event of the Columbia supercontinent. Moreover, the age of the Haizi diabase is roughly comparable with metallogenetic epoch of the typical iron-copper deposit, implying the possible metallogenetic significance of Late Paleoproterozoic magmatism in the southwestern Yangtze Block. This large-scale magmatic event might have been the main sources of ore-forming materials, such as Cu and Fe. In addition, the “Meidang Formation”should be older than the diabase that intruded it. Therefore, we propose that the so called“Meidang Formation”, which may be considered as the more ancient basement strata existed before continental extension of the Kunyang rift, should be included in Paleoproterozoic Tangdan Group.