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New insights into regional tectonics of the Indochina Peninsula inferred from Lower-Middle Jurassic paleomagnetic data of the Sibumasu Terrane

机译:从西布马苏地带的中下侏罗世古磁数据推论印度支那半岛区域构造的新见解

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摘要

The post-Jurassic occurrence of differential tectonic rotation between the Indochina and South Sundaland blocks remains an issue to be properly investigated. New paleomagnetic study is used here to find the role of Sibumasu Terrane in this rotation, which is located between a clockwise rotated Indochina Block and a counter-clockwise rotated South Sundaland Block. For this purpose, lower to middle Jurassic red sandstones of the Umphang Group in the Sibumasu Terrane were sampled at 21 sites in the Ratchaburi area (13.6°E, 99.6°E), Thailand. Stepwise thermal demagnetization by 680 ℃ unblocked a pre-folding characteristic remanent magnetization. A mean direction of this component at 100% unfolding is Ds = 348.5°, Is = 24.7°, α_(95) = 10.5°, k=10.7, N=20, corresponding to an Early-Middle Jurassic pole of λ = 78.6°N, φ= 10.6°E (A_(95) = 9.3). Comparison of this direction with those reported from other localities of the Umphang Group (Kalaw, Mae Sot and North Trang Syncline localities) reveal variable declinations (between 348.5° and 44.7°) for the Sibumasu Terrane. We ascribe this variation to differential tectonic deformation in the Sibumasu Terrane, as reflected from sinusoidal shaped structural features in the study area. The presence of such features in the granitic rocks indicates the occurrences of deformational activities after their intrusion, which took place in the period between 130 Ma and 51 Ma. The Sibumasu Terrane behaved as an independent fragment at a time when Indochina was undergoing a clockwise rotation and southward displacement, as a result of extrusion tectonics after the gigantic India-Asia collision. Taking into consideration a westerly deflected declination (D = 342.8°) from the West Trang area in Peninsular Thailand, a counterclockwise rotation of 15° is estimated for the Sibumasu Terrane, as a result of continuous northward indentation of the Australian Plate into South Sundaland Block.
机译:侏罗纪以后,印度支那和南桑达兰地区之间构造差异的旋转仍然是一个需要适当研究的问题。这里使用新的古磁研究来发现Sibumasu Terrane在此旋转中的作用,该旋转位于顺时针旋转的印度支那地块和逆时针旋转的南桑达兰地块之间。为此,在泰国Ratchaburi地区(东经13.6°,东经99.6°)的21个地点对Umphang组的中低侏罗纪侏罗纪红砂岩进行了采样。 680℃的逐步热退磁可消除预折叠特性的剩余磁化强度。该分量在100%展开时的平均方向为Ds = 348.5°,Is = 24.7°,α_(95)= 10.5°,k = 10.7,N = 20,对应于λ= 78.6°的中侏罗纪极点N,φ= 10.6°E(A_(95)= 9.3)。将此方向与Umphang组其他地区(Kalaw,Mae Sot和North Trang Syncline地区)报告的方向进行比较,发现西伯马苏地形的偏角变化较大(在348.5°至44.7°之间)。我们将这种变化归因于研究区域中正弦形结构特征所反映的西布马苏地带的不同构造变形。花岗岩中这种特征的存在表明它们侵入后发生了变形活动,这种活动发生在130 Ma至51 Ma之间。巨大的印度-亚洲碰撞后,由于挤压构造作用,印度支那正经历顺时针旋转和向南位移时,Sibumasu Terrane表现为一个独立的碎片。考虑到泰国半岛西董里地区的西偏偏角(D = 342.8°),由于澳大利亚板块不断向北凹入南桑达兰地块,Sibumasu Terrane估计逆时针旋转15° 。

著录项

  • 来源
    《Journal of Asian earth sciences》 |2014年第11期|126-138|共13页
  • 作者单位

    Department of Earth and Planetary Sciences, Faculty of Science, Kobe University, Kobe, Japan;

    Department of Geology, Faculty of Science, Taibah University, Madinah 41477, Saudi Arabia;

    Economic Geology Division, Department of Mineral Resources, Rama 6, Bangkok, Thailand;

    Economic Geology Division, Department of Mineral Resources, Rama 6, Bangkok, Thailand;

    Horizon Institute for Geology and Chronology Co., Ltd., Okayama 703-8252, Japan;

    Department of Earth and Planetary Sciences, Faculty of Science, Kobe University, Kobe, Japan;

    Department of Earth and Planetary Sciences, Faculty of Science, Kobe University, Kobe, Japan;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Sibumasu Terrane; Paleomagnetism; Jurassic; Tectonics; SE Asia;

    机译:Sibumasu Terrane;古磁性侏罗纪构造;东南亚;

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