| 根据深部地球物理资料和古板块构造格架重新厘定槽台界线 |
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| 引用本文： | 张振法.根据深部地球物理资料和古板块构造格架重新厘定槽台界线[J].内蒙古地质,1994(Z1). |
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| 作者姓名： | 张振法 |
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| 作者单位： | 内蒙古地矿局第一物化探队 |
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| 摘 要： | 大地电磁测深、地震测深、深部地球物理场特征和古板块构造格架表明，华北地台与蒙古—兴安古生代地槽褶皱区界线位于田水井—六驼山—温图高勒—巴音毛道—图克木—巴音查干—白音敖包—温都尔庙—那日图—西拉木伦构造线。从田水井向西，槽合界线进入准噶尔—塔里木板块构造区；从西拉木伦向东，槽台界线尖灭在松辽前寒武板块西南缘。
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| 关 键 词： | 地震测深，大地电磁测深，板块构造格架，华北地合，槽台界线。 |
Boundary of Geosyncline and Platform Redivided According to Deep Geophysical Data and Old Plate of Structural Framework |
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| Zhang Zhenfa.Boundary of Geosyncline and Platform Redivided According to Deep Geophysical Data and Old Plate of Structural Framework[J].Geology of Inner Mongolia,1994(Z1). |
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| Authors: | Zhang Zhenfa |
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| Institution: | Fist Physical chemical exploring team of Inner Mongolia |
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| Abstract: | The telluric electromagnetic sounding,earthquack sounding,deep geophysical fieldcharacter and old plate structural framework indicate that North China platform. Mongoli-a-Xingan Paleozoic Era geosyncline fold area boundary located to Tianshuijing-Luitu-oshan-Wentougaole-Bayinmaodao-Tukemu-Bayinchagen-Baiyinaobao-Wenduermiao-Naritu-Xilamuluen structural line.From Tianshuijing to west the boundary ofgeosyncline and platform enters Junggar,Tarim plate structural area;form Xilamulun toeast,boundary of platform and geosyncline taper out in west-south boundary of Songlaoprecambrian platform margin. |
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| Keywords: | earthquack sounding telluric electomagnetic sounding plate structural framework North China geosyucline and platform boundary |
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