| 中秦岭区断裂带波动效应探讨 |
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| 引用本文： | 李侠.中秦岭区断裂带波动效应探讨[J].陕西地质,1998(1). |
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| 作者姓名： | 李侠 |
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| 作者单位： | 西安工程学院!西安，710054 |
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| 摘 要： | 本文运用波浪镶嵌构造理论，讨论了中秦岭区由于几条主要断裂带相互欠替式的动“静”转化，使其间地块随之天平摆动及分“和”运动，从而导致了泥盆系发育的差异。
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| 关 键 词： | 东秦岭 泥盆系 波浪镶嵌构造 断裂动“静”转化 地块天平摆动及分“和”运动 |
DISCUSSION 0F WAVY EFFEST 0F SOME FAULTS IN THE MIDDLE QINLING |
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| Li Xia.DISCUSSION 0F WAVY EFFEST 0F SOME FAULTS IN THE MIDDLE QINLING[J].Geology of Shaanxi,1998(1). |
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| Authors: | Li Xia |
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| Abstract: | Based on the wavy mosaic tectonic hypothesis, the transition of some major faults fromthe active to inactive has been discussed in this paper. Such transitions led to the partitioningand coalescing, as well as the baIance-Iike oscillation of the biocks among those faults, andfurthermore, have rise to the difference of Devonian development. |
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| Keywords: | middle Qinling Devonian wavy mosaic transition of fault activities balance like oscillation |
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