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作 者:陈新跃[1] 王岳军[1] 韦牧[2] 范蔚茗[1] 彭头平[1]
机构地区:[1]中国科学院广州地球化学研究所同位素年代学和地球化学重点实验室 [2]福建省第八地质大队,福建龙岩364012
出 处:《大地构造与成矿学》2006年第3期312-319,共8页Geotectonica et Metallogenia
基 金:国家自然科学基金(40334039;40421303;40473019);中国科学院知识创新工程项目(KZCX1102)的联合资助.
摘 要:在海南岛西部公爱地区识别出NW向韧性剪切带,其野外构造解析和显微构造分析表明,公爱NW向韧性剪切带早期为右旋剪切,变形温度约300~450℃。对该韧性剪切带糜棱岩样品中白云母单矿物的40Ar39Ar定年结果表明:样品04HN17和04HN18分别给出了250.0±1.0Ma和248.0±1.0Ma的40Ar/39Ar坪年龄,为印支早期变形产物。海南公爱NW向韧性剪切带变形运动学和变形时序与印支北部NW向韧性剪切带(如SongMa地区)具有很好的一致性,这为理解公爱地区早中生代构造演化及华南陆块和印支半岛印支期构造演化提供了新的信息。All the structural and microstructural observations suggest the tectonic movement of dextral shearing for the NW-trending shear zones in Gong'ai region, Hainan Island. According to the quartz c-axis preferred orientations of three mylonitic rock samples in NW-trending shear zone and the feldspar-quartz micro-deformation structures of these samples, we presume that the deformational temperature is about 450℃ to 300℃. Muscovite, separated from sample 04HN17 and sample 04HN18, both mylonitic rocks samples from Gong'ai farmyard in NW-trending shear zones, yields well-defined ^40Ar-^39Ar plateau age of 250.0 ± 1.0Ma for about 87 % released ^39 Ar and 248.0± 1.0 Ma for about 68% released ^39Ar, respectively. These ages are interpreted to date cooling in terms of ^40Ar-^39Ar closure temperatures following synkinematic growth of muscovite as a consequence of mylonitic overprinting and deformation of NW-trending shear zones. The NW-trending shear zones in Gong'ai region are similar to the NW-trending shear zones in northern Indochina block ( such as Song Ma region) in kinematics and deformation epoch during early Indosinian. It can offer new information in regard to the early Mesozoic structural development of Gong'ai region in Hainan Island and the Indosinian structural development of Southern China and Indochina blocks.
关 键 词:NW向韧性剪切带 ^40AR-^39AR年代学 海南岛公爱地区
分 类 号:P542[天文地球—构造地质学] P597[天文地球—地质学]
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