摘要
对海南岛北西部戈枕地区侵位于古中元古代抱板群花岗质岩进行了CL成像制约下的SHRIMP锆石U—Pb年龄测定,获得了1455±12Ma的U—Pb谐和年龄、1454±12Ma有利的^207Pb/^206Pb中值年龄。结合该花岗质岩锆石内部结构、岩浆源区和变形变质特征,以及前人多种定年成果,认为该花岗质岩结晶年龄应为~1450Ma,随后于~1400Ma经历了一次构造-热变质事件;Rodinia超大陆聚合前,华夏地块(包括海南岛、或至少是海南岛北西部)最可能位于劳伦大陆南缘的西南延伸部分。研究结果还暗示华夏地块(包括海南岛)所经历的格林威尔造山事件可能较扬子地块偏早,古、中元古代抱板群沉积上限应约束在~1450Ma。
The Precambrian granitoid pluton emplaced in the Paleoproterozoic-Mesoproterozoic Baoban Group in Gezhen area, northwest Hainan Island, south China was dated by SHRIMP U-Pb analysis assisted by CL image. Zircon from the pluton yields a concordant SHRIMP U-Pb age of 1455 ± 12Ma with a weighted mean ^207pb/^206pb age of 1454 ± 12Ma, indicating its emplacement at -1450Ma. In connection with the zircon internal structure, the structural deformation/metamorphism and the provenance of the pluton, as well as the previously published age data by different dating methods, we suggest that a tectono-thermal metamorphic event most likely took place at - 1400 Ma, and thus the minimum depositional age for the Baoban Group should be ca. - 1450 Ma. Cathaysian Block (including Hainan Island, at least its northwest part) could be regarded as a southwestward extension of southern Laurentia before the assembly of the Mesoproterozoick-Neoproterozoic Rodinia supercontinent. Our research results also imply that Cathaysian Block ( including Hainan Island) probably underwent an earlier Grenville orogeny event, in comparison with Yangtze Block.
出处
《大地构造与成矿学》
EI
CAS
CSCD
北大核心
2006年第4期510-518,共9页
Geotectonica et Metallogenia
基金
国家自然科学基金项目(No.40473017)
中国科学院广州地球化学研究所所级创新项目(GIGCX04-4)联合资助.