Crustal deformation;
Volcano geodesy;
MATLAB;
Pressure source;
Augustine volcano;
LONG VALLEY CALDERA;
ELASTIC HALF-SPACE;
TENSILE FAULTS;
CALIFORNIA;
SHEAR;
D O I:
10.1016/j.jvolgeores.2012.12.018
中图分类号:
P [天文学、地球科学];
学科分类号:
07 ;
摘要:
We have developed a MATLAB software package for the most common models used to interpret deformation measurements near faults and active volcanic centers. The emphasis is on analytical models of deformation that can be compared with data from the Global Positioning System (GPS), InSAR, tiltmeters and strainmeters. Source models include pressurized spherical, ellipsoidal and sill-like magma chambers in an elastic, homogeneous, flat half-space. Dikes and faults are described following the mathematical notation for rectangular dislocations in an elastic, homogeneous, flat half-space. All the expressions have been checked for typographical errors that might have been present in the original literature, extended to include deformation and strain within the Earth's crust (as opposed to only the Earth's surface) and verified against finite element models. A set of GPS measurements from the 2006 eruption at Augustine Volcano (Alaska) is used to test the software package. The results show that the best fit source to the GPS data is a spherical intrusion (Delta V = 5 x 10(-4) km(3)), about 880 m beneath the volcano's summit. (C) 2012 Elsevier B.V. All rights reserved.
机构:
US Geol Survey, David A Johnston Cascades Volcano Observ, Vancouver, WA 98683 USAUS Geol Survey, David A Johnston Cascades Volcano Observ, Vancouver, WA 98683 USA
机构:
US Geol Survey, David A Johnston Cascades Volcano Observ, Vancouver, WA 98683 USAUS Geol Survey, David A Johnston Cascades Volcano Observ, Vancouver, WA 98683 USA