首页|Fractalness of land gravity data and residual isostatic anomalies map of Argentina, Chile and western Uruguay

Fractalness of land gravity data and residual isostatic anomalies map of Argentina, Chile and western Uruguay

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Gravity anomalies are often strongly influenced by topography, which effect is mitigated through appropriate reductions. Usually, a standard value of 2670 kg/m(3) is used for the density of topography in the absence of specific information. However, various methods have been implemented to obtain density of topography estimates directly from the gravity data. A particularly suitable technique for regional scale studies is based on analyzing the fractal nature of gravity anomalies for a particular region.

gravity anomaliesfractal geometryisostatic residuals

Alicia Miranda, Silvia、Hector Herrada, Alfredo、Cristina Pacino, Maria

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Univ Nacl San Juan, Dept Geofis & Astron FCEFN, RA-5400 Rivadavia, San Juan, Argentina

Univ Nacl San Juan, Dept Ingn Agrimensura FI, RA-5400 San Juan, Argentina

Univ Nacl Rosario, Fac Ciencias Exactas Ingn & Agrimensura, CONICET, RA-2000 Rosario, Santa Fe, Argentina

2015

Geofisica internacional

Geofisica internacional

SCI
ISSN：0016-7169
年,卷(期)：2015.54(4)
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