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首页> 外文期刊>Gondwana research: international geoscience journal >Late Paleozoic paleomagnetism of South Mongolia: Exploring relationships between Siberia, Mongolia and North China
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Late Paleozoic paleomagnetism of South Mongolia: Exploring relationships between Siberia, Mongolia and North China

机译:蒙古晚期古生代古构造论:探索西伯利亚,蒙古与华北之间的关系

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The tectonic evolution of a large region that includes South Siberia, Mongolia and North China is still a matter of fierce debate. This is due, at least in part, to the contentious proposals detailing the kinematics of the major tectonic units in that area. One solution to the problem is the acquisition of better defined paleomagnetic data for the various players in the system. We carried out a paleomagnetic study of Early Carboniferous subduction-related volcanic rocks of the Trans-Altai zone in South Mongolia and successfully isolated a pre-folding and presumably primary component from 22 sites. A critical analysis of Late Paleozoic paleomagnetic data from Mongolia revealed several problematic data sets, while the paleolatitudes derived from more reliable studies agreed well with the expected values for Siberia and were consistently different from those for the North China block. We also found that Late Paleozoic declinations from Mongolia are rotated counterclockwise through various angles with respect to Siberia. In addition, those rotations are widespread in both Inner Mongolia and the North China block. In this paper, we put forward some testable hypotheses and propose a preliminary paleogeographic scheme of the region: 1) Consistent difference in Late Paleozoic paleolatitudes between Siberia and Mongolia on the one hand and the North China block on the other, is largely due to strong inclination shallowing in paleomagnetic data for the latter area, where most data are from sedimentary rocks. 2) Widespread counterclockwise rotations in Mongolia, Inner Mongolia and North China may be accounted for by a wide zone of sinistral transpression that was active in the Early Mesozoic. 3) In the Early Mesozoic, the Mongol-Okhotsk Ocean was much narrower than is usually assumed; 4) There was no large-scale oroclinal bending between Siberia and North China in the Permian-Early Mesozoic. (C) 2016 International Association for Gondwana Research. Published by Elsevier B.V. All rights reserved.
机译:包括南西伯利亚,蒙古和华北在内的大区域的构造演化仍然是激烈的辩论问题。这至少部分是由于有争议的提案详细说明了该地区主要构造单元的运动学。解决该问题的一种方法是为系统中的各个角色获取定义更好的古磁数据。我们对蒙古南部的Trans-Altai地区与早期石炭纪俯冲有关的火山岩进行了古磁研究,并成功地从22个地点中分离出了一个可能是褶皱的主要成分。对来自蒙古的晚古生代古磁数据的批判分析揭示了一些有问题的数据集,而从更可靠的研究中得出的古纬度与西伯利亚的预期值非常吻合,并且与华北地块的预期值始终存在差异。我们还发现,来自蒙古的古生代晚期偏斜相对于西伯利亚逆时针旋转了不同角度。此外,这些轮换在内蒙古和华北地区均很普遍。在本文中,我们提出了一些可检验的假设,并提出了该地区的初步古地理方案:1)西伯利亚和蒙古和华北地块一方面在晚古生代古纬度上保持一致,这在很大程度上是由于后一个地区的古磁数据中的倾斜变浅,其中大部分数据来自沉积岩。 2)蒙古,内蒙古和华北地区广泛的逆时针旋转可能是由早期中生代活跃的广泛的左旋压抑带引起的。 3)在中生代早期,蒙古-鄂霍次克海比通常认为的要狭窄得多; 4)在二叠纪-早中生代,西伯利亚和华北之间没有大规模的口斜。 (C)2016国际冈瓦那研究协会。由Elsevier B.V.发布。保留所有权利。

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