Zobrazeno 1 - 7
of 7
pro vyhledávání: '"Leshou, Chen"'
Autor:
Nelson, K. D., Zhao, Wenjin, Brown, L. D., Kuo, J., Che, Jinkai, Liu, Xianwen, Klemperer, S. L., Makovsky, Y., Meissner, R., Mechie, J., Kind, R., Wenzel, F., Ni, J., Nabelek, J., Leshou, Chen, Tan, Handong, Wei, Wenbo, Jones, A. G., Booker, J., Unsworth, M., Kidd, W. S. F., Hauck, M., Alsdorf, D., Ross, A., Cogan, M., Wu, Changde, Sandvol, E., Edwards, M.
Publikováno v:
Science, 1996 Dec 01. 274(5293), 1684-1688.
Externí odkaz:
https://www.jstor.org/stable/2890941
Autor:
Alan G. Jones, Ming Deng, David Kay, K. D. Solon, John R. Booker, Brian Roberts, Martyn Unsworth, Handong Tan, Doug Nelson, Paul A. Bedrosian, Leshou Chen, Wenbo Wei, Sheng Jin, Juanjo Ledo, Shenghui Li
Publikováno v:
Science. 292:716-719
Magnetotelluric exploration has shown that the middle and lower crust is anomalously conductive across most of the north-to-south width of the Tibetan plateau. The integrated conductivity (conductance) of the Tibetan crust ranges from 3000 to greater
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::7fc7dc22fa86a952148806e556757a3e
https://doi.org/10.1126/science.1010580
https://doi.org/10.1126/science.1010580
Publikováno v:
Science in China Series D: Earth Sciences. 40:269-275
Using the boundary element method, the numerical modeling problem of three-dimensional terrain effect on magnetotelluric (MT) field is solved. This modeling technique can be run on PC in the case of adopting special net division. The result of modeli
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::212779e4b410d334b64ff4dc8951ff6d
https://doi.org/10.1007/bf02877535
https://doi.org/10.1007/bf02877535
Publikováno v:
Chinese Science Bulletin. 42:764-767
THE modeling of 2-D terrain effect on magnetotelluric (MT) has been solved using finite ele-ment method (FEM) and boundary element method (BEM).This note uses BEM tosolve the problem. The solution of Hx - and Ex -polarization wave can be obtained by
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::661d007a16ed3379fc904c3c2098df16
https://doi.org/10.1007/bf03186973
https://doi.org/10.1007/bf03186973
Publikováno v:
Science. 274:1694-1696
The crust north of the Himalaya is generally electrically conductive below depths of 10 to 20 km. This conductive zone approaches the surface beneath the Kangmar dome (dipping north) and extends beneath the Zangbo suture. A profile crossing the north
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::46a4c8c22eb7faefd89a99b80faf27ac
https://doi.org/10.1126/science.274.5293.1694
https://doi.org/10.1126/science.274.5293.1694
Autor:
Unsworth MJ; Department of Physics, University of Alberta, Edmonton, Alberta, T6G 2J1, Canada. unsworth@phys.Ualberta.ca, Jones AG, Wei W, Marquis G, Gokarn SG, Spratt JE, Bedrosian P, Booker J, Leshou C, Clarke G, Shenghui L, Chanhong L, Ming D, Sheng J, Solon K, Handong T, Ledo J, Roberts B
Publikováno v:
Nature [Nature] 2005 Nov 03; Vol. 438 (7064), pp. 78-81.
Autor:
Chen L; Leshou Chen, Wenbo Wei, Handong Tan, China University of Geosciences, Beijing, China. J. R. Booker, Nong Wu, M. J. Unsworth, School of Geophysics, University of Washington, Seattle, WA 98195, USA. A. G. Jones, Geological Survey of Canada, 1 Observatory Crescent, Ottawa, Ontario, Canada K1A 0Y3., Booker JR, Jones AG, Wu N, Unsworth MJ, Wei W, Tan H
Publikováno v:
Science (New York, N.Y.) [Science] 1996 Dec 06; Vol. 274 (5293), pp. 1694-6.