首页> 外文会议>International GeologicalCongress >Diachronous Uplift along the Ailao Shan-Red River Left-lateral Strike-slip Shear Zone in the Miocene and Its Tectonic Implication, Yunnan, China
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Diachronous Uplift along the Ailao Shan-Red River Left-lateral Strike-slip Shear Zone in the Miocene and Its Tectonic Implication, Yunnan, China

机译:沿着北尚山红河左侧防滑剪剪区域的二次隆起及其构造构造,云南,云南

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The Ailao Shan-Red River metamorphic belt in southern Yunnan province, China, was one of the largest left-lateral,ductil strike-slip shear zone developed during the mid-Tertiary in Asia, To better understand the nature and timing of this feature, wAr/3'1Ar age spectrum and fission track analyses were undertaken on 18 K-feldspars and 4 apatites from seven sampling sites (including three sections of cross metamorphic belt) from Yuanyang to Zhelong for about 225 km along this belt. Using the MDD model (Multiple-Diffusion Domain model) these results yield 18 curves of cooling history in the temperature range from 400 - 150 °C. The common characteristics of these curves were to have one (or two) rapid cooling (>100 °C/Ma), rapid uplift event, in the age range from 25.7 - 17.8 Ma. The fission track ages range from 10.6 to 5.61 Ma. Both results indicate dicreasing from SE to NW along the shear zone. When ploted as a function of distance along the range, the starting time of rapid uplift and the fission track ages are getting younger linearly from Yuanyang (SE) to Zhelong (NW) at the slope of 34mm/yr and 30 mm/yr respec-tively. The surprising linear correlation can be interpreted by two probable tectonic models in different time ranges: (1) the slope of 34 mm/yr was probably just the speed of left-lateral strike-slip movement with uplift (slope angle of about 11°) and the starting lime of the rapid uplift decrease linearly during 25.7 to 17,8 Ma from SE to NW; (2) The slope of 30 mm/yr was considered a homogeneous extended speed of tectonic uplift from SE to NW during 10 Ma (or 15.5 Ma) to 5,5 Ma, propably due to a resistance of unfree interface at the SE edge of the shear zone. These results also support that a 15,5 Ma unconformity separates a younger left-lateral transpressional regime from an older left-lateral transtensional regime in the Red River shear zone in the Tonkin Gulf, Vietnam.
机译:中国南部南部的北山红河变质腰带是亚洲中等学区中最大的左侧左侧左侧左侧锯道滑动剪切区之一,更好地了解了这个功能的性质和时间,战争/ 3'1AR年龄频谱和裂变轨道分析是由18 k-feldspars和4位从yuanyang到Zelong的七个抽样网站(包括三个横向变质带)沿着这带距离Zelong的七个磷灰石和裂变轨道分析。使用MDD模型(多扩散域模型)这些结果在400-150°C的温度范围内产生18条冷却历史曲线。这些曲线的常见特征是具有一(或两种)快速冷却(> 100℃/ mA),快速提升事件,年龄范围为25.7-17.8 mA。裂变轨道年龄在10.6至5.61 mA的范围内。这两个结果表明从SE沿着剪切区的NW取代。当作为沿范围距离的距离绘制时,快速隆起的起始时间和裂变轨道年龄在34mm / Yr的斜率下从yuanyang(se)线性地线性地线性(nw)和30 mm / yr respec-恍惚。令人惊讶的线性相关性可以在不同时间范围内通过两个可能的构造模型来解释:(1)34 mm / yr的斜率可能只是左侧滑动运动的速度升高(斜率约11°)从SE到NW的25.7至17,8 mA期间,快速隆起的起始石灰在25.7至17,8 ma期间降低; (2)30mm / Yr的斜率被认为是在10 mA(或15.5mA)至5.5mA期间的均匀延伸的构造隆起速度从SE到NW,并且由于在SE边缘处的未自由界面的电阻是由于未满的界面的电阻剪切区。这些结果还支持15.5 mA的无关​​,从越南Tonkin海湾的红河剪切区中的较旧的左侧横向静音制度分开了一个较小的左侧横向静音制度。

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