An Adaptive 2D Planar Projection and Its Application in Geoscience Studies

Yong Zheng , Bikai Jin , Xiong Xiong , Sidao Ni

Journal of Earth Science ›› 2015, Vol. 26 ›› Issue (5) : 724 -728.

PDF
Journal of Earth Science ›› 2015, Vol. 26 ›› Issue (5) : 724 -728. DOI: 10.1007/s12583-015-0591-2
Article

An Adaptive 2D Planar Projection and Its Application in Geoscience Studies

Author information +
History +
PDF

Abstract

A linear projection approach is developed to present geoscience research result in planar coordinate system projected from spherical coordinate system. Here, the sphere is intersected by a plane and its surface is projected onto the plane. In order to keep the projected coordinate system orthogonal, and minimize the distortion, one axis of the planar coordinate system is chosen in our projection based on the shape of the region to be projected, and the other axes can be chosen arbitrarily or based on the constraint of the orthogonality. In the new method the projection is self-contained. The forward projection can be fully projected backward without loss of precision. The central area of the sphere will be projected to the planar system without distortion, and the latitudinal length in the rotated spherical system keeps constant during the projecting process. Only the longitudinal length in the rotated spherical system changes with the rotated latitude. The distortion of the projection therefore, overall, is small and suitable for geoscience studies.

Keywords

adaptive 2D projection / linear / planar / geoscience

Cite this article

Download citation ▾
Yong Zheng, Bikai Jin, Xiong Xiong, Sidao Ni. An Adaptive 2D Planar Projection and Its Application in Geoscience Studies. Journal of Earth Science, 2015, 26(5): 724-728 DOI:10.1007/s12583-015-0591-2

登录浏览全文

4963

注册一个新账户 忘记密码

References

[1]

England P., Molnar P. Active Deformation of Asia: From Kinematics to Dynamics. Science, 1997, 278(5338): 647-650.

[2]

Flesch L. M., Haines A. J., Holt W. E. Dynamics of the India-Eurasia Collision Zone. Journal of Geophysical Research, 2001, 106 B8 16435

[3]

Kirby J. F., Swain C. J. Mapping the Mechanical Anisotropy of the Lithosphere Using a 2D Wavelet Coherence, and Its Application to Australia. Physics of the Earth and Planetary Interiors, 2006, 158(2–4): 122-138.

[4]

Geochemistry, Geophysics, Geosystems, 2008, 9 3

[5]

Journal of Geophysical Research, 2009, 114 B8

[6]

Kong X., Yin A., Harrison T. M. Evaluating the Role of Preexisting Weaknesses and Topographic Distributions in the Indo-Asian Collision by Use of a Thin-Shell Numerical Model. Geology, 1997, 25(6): 527-530.

[7]

Ma H. S., Zheng Y., Shao Z. G., . Simulation on Seismogenic Environment of Strong Earthquakes in Sichuan-Yunnan Region, China. Concurrency and Computation: Practice and Experience, 2009, 22(12): 1626-1643.

[8]

Meade B. J. Present-Day Kinematics at the India-Asia Collision Zone. Geology, 2007, 35 1 81

[9]

Royden L. H. Surface Deformation and Lower Crustal Flow in Eastern Tibet. Science, 1997, 276(5313): 788-790.

[10]

Snyder J. P. Map Projections—A Working Manual. U.S. Geological Survey Professional Paper 1395, 1987

[11]

Geophysical Research Letters, 2006, 33 2

[12]

Zheng Y., Xiong X., Chen Y., . Effects of Fault Movement and Material Properties on Deformation and Stress Fields of Tibetan Plateau. Earthquake Science, 2011, 24(2): 185-197.

[13]

Zheng Y., Chen Y., Fu R. S., . Simulation of the Effects of Faults Movement on Stress and Deformation Fields of Tibetan Plateau by Discontinuous Movement Models. Chinese J. Geophys., 2007, 50(5): 1398-1408.

[14]

Zheng Y., Fu R. S., Xiong X. Dynamic Simulation of Lithospheric Evolution from the Modern China Mainland and Its Surrounding Areas. Chinese J. Geophys., 2006, 49(2): 415-427.

AI Summary AI Mindmap
PDF

119

Accesses

0

Citation

Detail

Sections
Recommended

AI思维导图

/