首页> 外文期刊>Science in China, series B. Chemistry,Life Sciences and Earth Sciences >Palaeomagnetic record from RH lacustrine core in Zoige Basin of Tibetan Plateau
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Palaeomagnetic record from RH lacustrine core in Zoige Basin of Tibetan Plateau

机译:青藏高原若尔盖盆地RH湖相岩心的古地磁记录

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摘要

RH core, located in the Zoige Basin of Eastern Tibetan Plateau, is a quite good lacustrine core. It is 120,40m long. Nine geomagnetic excursions or events were recorded in the core during Brunhes normal epoch based on measurement results of the remnant magnetization of small interval core samples (10 cm interval) under series AF demagnetization, and organic carbon-14 and AMS dates. The excursions recorded by the core can be correlated with those found in other regions in the world. They are the mostdetailed record in lacustrine deposit in China. B/M boundary in the core is at the depth of 108.0m. It can be calculated from the depositional rate of 0.13 mm/a that the bottom age of the core is 825 ka B.P. The excursion ages in Brunhes and their correlation with those found in other regions are discussed.
机译:RH核心位于青藏高原东部的Zoige盆地,是一个相当不错的湖泊核心。长120,40m。根据连续AF退磁过程中小间隔岩心样本(间隔为10 cm)的剩余磁化强度的测量结果,在Brunhes正常时期记录了9次地磁偏移或事件在岩心中的记录。核心记录的游览可以与世界其他地区的游览相关联。它们是中国湖泊沉积最详细的记录。岩心中的B / M边界位于108.0m的深度。从0.13mm / a的沉积速率可以计算出芯的底部年龄为825ka B.P.。讨论了布鲁日(Brunhes)的游览年龄及其与其他地区的游览年龄的相关性。

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