“Smith’s rule”的概念、定义、翻译、参考文献-科学参考

Smith’s rule

Geology and Earth Sciences

The formula by which the maximum possible depth of a body of unknown shape can be determined using gravity data. The body can have either a positive or negative density contrast with the surrounding rocks. The maximum depth, d_max, is given by: d_max = Ag_max/(δ‎g/δ‎x), where δ‎g/δ‎x is the maximum horizontal gradient of the gravity anomaly, g_max is the value of the anomaly peak, and A varies between 0.86 for a three-dimensional body to 0.65 for an essentially two-dimensional body.

单词	Smith’s rule
释义	Smith’s rule Geology and Earth Sciences The formula by which the maximum possible depth of a body of unknown shape can be determined using gravity data. The body can have either a positive or negative density contrast with the surrounding rocks. The maximum depth, d_max, is given by: d_max = Ag_max/(δ‎g/δ‎x), where δ‎g/δ‎x is the maximum horizontal gradient of the gravity anomaly, g_max is the value of the anomaly peak, and A varies between 0.86 for a three-dimensional body to 0.65 for an essentially two-dimensional body.
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