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首页> 外文期刊>Earth and Planetary Science Letters: A Letter Journal Devoted to the Development in Time of the Earth and Planetary System >Paleomagnetic results from the lower Mesozoic Daedong Supergroup in the Gyeonggi Block, Korean Peninsula: an eastern extension of the South China Block
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Paleomagnetic results from the lower Mesozoic Daedong Supergroup in the Gyeonggi Block, Korean Peninsula: an eastern extension of the South China Block

机译:古磁的结果来自朝鲜半岛京畿道中下生代大同超群:华南地块的东部延伸

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摘要

Lower Mesozoic lake deposits in the Daedong Supergroup of the Gyeonggi Block were collected at 38 sites for paleomagnetic study. A remanent magnetization component with unblocking temperatures of 635-660 ℃ (component A) was isolated from four sites. The directions of this component with both normal and reversed polarities yielded positive fold and reversal tests at the 95% confidence level. Component A is interpreted to be of primary origin of Late Triassic time. The mean direction of component A (D = 82.2°, I = 23.1° with α_(95) = 4.1°), together with previously reported primary directions, yields a pole representative for the Gyeonggi Block at 31.9°N, 220.2°E (A_(95) = 12.7°). The paleomagnetic pole shows good agreement with that for the South China Block, suggesting that the Gyeonggi Block has been part of the South China Block. The Gyeonggi Block, as the eastern part of the South China Block, is regarded to have thrust to its position at the present Korean Peninsula during the collision between the North and South China Blocks.
机译:京畿道大同超群的下中生界湖沉积物被收集到38个地点用于古磁研究。从四个位置分离出具有635-660℃畅通温度的剩磁成分(成分A)。极性为正向和反向的该组件的方向在95%置信度下均产生正向折叠和反向测试。组分A被解释为晚三叠世的主要起源。分量A的平均方向(D = 82.2°,I = 23.1°,α_(95)= 4.1°)以及先前报告的主要方向,在31.9°N,220.2°E时代表了京畿道的极点( A_(95)= 12.7°)。古磁极与华南地块具有很好的一致性,表明京畿道已成为华南地块的一部分。京畿道作为华南街区的东部,在华北街区与华南街区发生碰撞时被认为已推向现在的朝鲜半岛。

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