| 重力归一化总梯度及其相位的叠置方法研究 |
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| 引用本文： | 吴燕冈,鲁新便.重力归一化总梯度及其相位的叠置方法研究[J].世界地质,1996,15(3):84-90. |
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| 作者姓名： | 吴燕冈 鲁新便 |
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| 作者单位： | [1]长春地质学院地球物理系 [2]地矿部西北石油地质局 |
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| 摘 要： | 通过理论推导和模型实验证明：将重力归一化总梯度及其相位二者相叠置的方法，用于确定壳内深大断裂的空间位置是准确可行的。在实际资料处理地，将该方法应用于新疆横穿塔里木盆地及其周缘造山带的大红柳滩－老虎台条带域，划分出盆地的边界和多条深大断裂。对各种参数的影响和选择做了深入的探讨。
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| 关 键 词： | 重力测量 重力归一化 相位 叠置法 |
A Study of Appending of Total Gradient of Gravity and its Phase |
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| Wu Yangang ,Shan Rujian,Zhou Fuxiang.A Study of Appending of Total Gradient of Gravity and its Phase[J].World Geology,1996,15(3):84-90. |
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| Authors: | Wu Yangang Shan Rujian Zhou Fuxiang |
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| Abstract: | It is feasible to determine the location of large and deep faults in the crustby means of appending normalized total gradient of gravity and its phase. To made use ofthe way, a zonal region from Dahongliutan to Laohutai crossing the Talimu Basin inXinjiang Autonomous Region is determined,and the boundaries of the basin and severaldeep faults is divided. At the same, some efflects and choices of various parameters arethoroughly discussed in the paper. |
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| Keywords: | gradient of gravity gravity phase parameter |
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