Toolbox for Analysis of Flexural Isostasy (TAFI)-A MATLAB toolbox for modeling flexural deformation of the lithosphere

被引:10
|
作者
Jha, Sumant [1 ]
Harry, Dennis L. [1 ]
Schutt, Derek L. [1 ]
机构
[1] Colorado State Univ, Dept Geosci, 1482 Campus Delivery, Ft Collins, CO 80523 USA
来源
GEOSPHERE | 2017年 / 13卷 / 05期
基金
美国国家科学基金会;
关键词
EFFECTIVE ELASTIC THICKNESS; OCEANIC LITHOSPHERE; TRANSANTARCTIC MOUNTAINS; CONTINENTAL LITHOSPHERE; GRAVITY-ANOMALIES; T-E; UPLIFT; RIGIDITY; STRENGTH; STRESS;
D O I
10.1130/GES01421.1
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
This paper describes a new interactive toolbox for the MATLAB computing platform called Toolbox for Analysis of Flexural Isostasy (TAFI). TAFI supports two-and three-dimensional (2-D and 3-D) modeling of flexural subsidence and uplift of the lithosphere in response to vertical tectonic loading. Flexural deformation is approximated as bending of a thin elastic plate overlying an inviscid fluid asthenosphere. The associated gravity anomaly is calculated by summing the anomalies produced by flexure of each density interface within the lithosphere, using Parker's algorithm. TAFI includes MATLAB functions provided as m-files (also called script files) to calculate the Green's functions for flexure of an elastic plate subjected to point or line loads, and functions to calculate the analytical solution for harmonic loads. Numerical solutions for flexure due to non-impulsive 2-D or 3-D loads are computed by convolving the appropriate Green's function with a spatially discretized load function read from a user-supplied file. TAFI uses MATLAB's intrinsic functions for all computations and does not require any other specialized toolbox, functions, or libraries except those distributed with TAFI. The modeling functions within TAFI can be called from the MATLAB command line, from within user-written programs, or from a graphical user interface (GUI) provided with TAFI. The GUI facilitates interactive flexural modeling and easy comparison of the model to gravity observations and to data constraining flexural subsidence and uplift.
引用
收藏
页码:1555 / 1565
页数:11
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