The forward computation and inversion of magnetotelluric fields in two-dimensional nonisotropic medium

2015 ◽  
Author(s):  
Miaoxin Yang ◽  
Handong Tan ◽  
Xiaohong Meng ◽  
Changhong Lin
1992 ◽  
Vol 203 (1-4) ◽  
pp. 305-324 ◽  
Author(s):  
J.D. van Wees ◽  
K. De Jong ◽  
S. Cloetingh

2008 ◽  
Vol 63 (8) ◽  
pp. 954-962 ◽  
Author(s):  
Virginia Lozano ◽  
Matthias Freytag ◽  
Peter G. Jones ◽  
Armand Blaschette

This study characterizes the supramolecular synthons that dominate the interionic organization of 3-bromoanilinium di(4-bromobenzenesulfonyl)amide (1) and the corresponding 4-bromoanilinium salt (2) in their respective crystal structures (1: orthorhombic, Pbca, Z´ = 1; 2: monoclinic, P21/n, Z´ = 1). Although these compounds contain N+-H donors and C-Br groups in equal numbers, their ion packings are exclusively governed by classical, and mostly bifurcated, hydrogen bonds of the type N+-H···O=S/N−, whereas halogen bonding C-Br···O=S/N− is absent from both structures. The isomerism of the cations, which is the only chemical difference between 1 and 2, drives the hydrogen bonds to form a network that is two-dimensional in 1, but one-dimensional in 2. The resulting layers or strands are coherently built up from hydrophilic internal regions consisting of NH3 + and (SO2)2N− groups, external hydrophobic domains of phenyl rings, and peripherically projecting bromine atoms. As the hydrophobic groups from adjacent layers or strands do not interdigitate, the bromine atoms are sterically available to form short Br・ ・ ・Br interlayer contacts of quasi-type I in 1 and inversion symmetric Br4 interstrand quadrilaterals in 2. The results of a database search for quadrilateral (C-Br)4 synthons are also presented.


2015 ◽  
Vol 64 (9) ◽  
pp. 099301
Author(s):  
Fan Yi-Ren ◽  
Wu Fei ◽  
Li Hu ◽  
Huo Ning-Ning ◽  
Wang Yao-Sen ◽  
...  

2021 ◽  
Vol 2005 (1) ◽  
pp. 012008
Author(s):  
Zhu Gao ◽  
Runlin Luo ◽  
XianLi Xiang ◽  
Zhengxia Xia ◽  
Zhifeng Zhao

Geophysics ◽  
1993 ◽  
Vol 58 (5) ◽  
pp. 637-644 ◽  
Author(s):  
John Mariano ◽  
William J. Hinze

A method has been devised for the forward computation of magnetic anomalies due to two‐dimensional (2-D) polygonal bodies with heterogeneously directed magnetization. The calculations are based on the equivalent line source approach wherein the source is subdivided into discrete elements that vary spatially in their magnetic properties. This equivalent dipole line method provides a fast and convenient means of representing and computing magnetic anomalies for bodies possessing complexly varying magnitude and direction of magnetization. The algorithm has been tested and applied to several generalized cases to verify the accuracy of the computation. The technique has also been used to model observed aeromagnetic anomalies associated with the structurally deformed, remanently magnetized Keweenawan volcanic rocks in eastern Lake Superior. This method is also easily adapted to the calculation of anomalies due to two and one‐half‐dimensional (2.5-D) and three‐dimensional (3-D) heterogeneously magnetized sources.


Author(s):  
Samuel Bignardi ◽  
Francesco Fedele ◽  
Anthony Yezzi ◽  
Glenn Rix ◽  
Giovanni Santarato

Geophysics ◽  
1990 ◽  
Vol 55 (7) ◽  
pp. 914-919 ◽  
Author(s):  
J. Dellinger ◽  
J. Etgen

Until recently, the term “elastic” usually implied two‐dimensional (2-D) and isotropic. In this limited context, the divergence and curl operators have found wide use as wave separation operators. For example, Mora (1987) used them in his inversion method to allow separate correlation of P and S arrivals, although the separation is buried in the math and not obvious. Clayton (1981) used them explicitly in several modeling and inversion methods. Devaney and Oristaglio (1986) used closely related operators to separate P and S arrivals in elastic VSP data.


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