4. Gravity Anomalies and the Corresponding Crustal Structure.(Part 1) : Numerical Tables Useful in Three-Dimensional Gravity Interpretations

概要

論文の詳細を見る
A function Φ which was first introduced by Tsuboi and Tomoda and which gives surface mass density at square grid points over a horizontal underground surface at a depth D below the earth's surface corresponding to unit gravity at (x=y=0) and zero anomaly at all other grid points on the earth's surface is given by (1) below. This double integral is transformed to a single integral and then evaluated for D=0.01, 0.02, ・・・, 0.99 and 1.00.地表の原点x=y=0で1,他の格子点では0というような重力値を与える,深さDの所にある水平面上の質量の分布は,坪井・友田の導いた函数Φ(x,y,D)によつて与えられる.Φに含まれている二重積分を一重積分に直し,x,y=0,1,2・・・,10,D(格子間隔を単位にした深さ)=0.01,0.02,・・・,0.99,1.00についてΦを計算した.
1964-05-30