Paleomagnetic and rock magnetic investigations of the Changxing Permian‐Triassic section, Zhejiang Province, China
Paleomagnetic and rock magnetic investigations of the Changxing Permian‐Triassic section, Zhejiang Province, China
复制标题
浙江长兴二叠系—三叠系剖面古地磁及岩石磁学研究
DOI：
10.1029/93gl01242
复制
发表时间：
1993
影响因子：
5.2
通讯作者：
H. Mauritsch
中科院分区：
文献类型：
--
作者：
J. Dobson;F. Heller;Zheng‐Xiang Li;H. Mauritsch
对长兴县二叠系-三叠系类型剖面中的三叠系银坑组和二叠系长兴组进行的古地磁和岩石磁学实验表明，早三叠世白云岩样品中分离出高温主方向，而晚二叠世灰岩样品在侏罗纪表现为重新磁化。该剖面以前报道的长兴组的二叠纪-三叠纪极点(Lin等人，1985)与本研究的结果或扬子地块该时间段的其他极点不一致，可能是重新磁化的。
Paleomagnetic and rock magnetic experiments on the Triassic Yinkeng Formation and the Permian Changxing Formation sampled from the Permian-Triassic type section, Changxing County, reveal that a high temperature primary direction is isolated in dolomitic samples from the Early Triassic but the Late Permian limestones samples appear to be remagnetized during the Jurassic. A Permian-Triassic pole previously reported for the Changxing Formation from this section (Lin et al., 1985) is not in agreement with results from this study or other poles for that time interval reported for the Yangtze Block and may be remagnetized.
DOI：
10.1098/rspa.1953.0064
发表时间：
1953-01-01
影响因子：
--
作者：
FISHER, R
通讯作者：
FISHER, R