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苏南地区早、中泥盆世古地磁特征初步探讨
引用本文:翟永建,谭承泽,洪炎坤,杜齐. 苏南地区早、中泥盆世古地磁特征初步探讨[J]. 物探与化探, 1987, 11(5): 358-363
作者姓名:翟永建  谭承泽  洪炎坤  杜齐
作者单位:武汉地质学院北京研究生部(翟永建,谭承泽),地质矿产部南京石油物探研究所(洪炎坤),华东石油地质局第六物探大队(杜齐)
摘    要:我们对江苏南部中、下泥盆统茅山砂岩进行了古地磁初步研究.结果表明:(1)杨子地块早、中泥盆世时期处于赤道附近;(2)在晚侏罗一早白垩世期间,宁镇山脉相对于无锡地区顺时针水平旋转了37.5°,茅山山脉在晚白垩世相对无锡地区逆时针水平旋转了30.7°,(3)宁镇和茅山地区茅山砂岩的层位,似应上升到无锡地区茅山砂岩的上段中、下部.


A PRELIMINARY DISCUSSION ON PALEOMAGNETIC CHARACTERISTICS OF THE EARLY-MIDDLE DEVONIAN STRATA IN SOUTHERN JIANGSU
Affiliation:1. Beijing Graduate School, Wuhan College of Geology;
2. Nanjing Institute of Geophysical Prospecting for Petroleum, MGMR;
3. No. 6 Geophysical Prospecting Party, East China Eureau of Petroleum Geology
Abstract:Preliminary paleomagnetic studies have been conducted on the Middle-Lo wer Devonian Maoshan sandstone in southern Jiangsu. The result shows: (1) the Yangtze massif was located near the equator during the Early-Middle Devo nian; (2) the Ningzhen mountain range had a clockwise horizontal rotation of 37.5°relative to Wuxi area during the Late Jurassic-Early Cretaceous, while the Maoshan mountain range performed a counterclockwise horizontal rotation of 30.7°relative to Wuxi area in the Late Cretaceous; (3) it seems that the stratigraphic horizon of Maoshan sandstone in Ningzhen and Maoshan areas shou ld be raised somewhat so as to correspond to the middle and lower part of Upper Member of Maoshan sandstone in Wuxi area.
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