Crustal weakening and transgressive melt penetrative intrusion across the Kunlun Shan inferred from INDEPTH Phase III and Phase IV magnetotelluric data

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ADS bibcode: 2011AGUFM.T43A2300L
year: 2011
Listed Authors: Le Pape, F.; Jones, A. G.; Vozar, J.; Wei, W.; Dong, H.; Unsworth, M. J.; Jin, S.; Ye, G.; Jing, J.; Zhang, L.; Xie, C.
Listed Institutions: Geophysics Section, Dublin Institute for Advanced Studies, Dublin, Ireland;; Geophysics Section, Dublin Institute for Advanced Studies, Dublin, Ireland;; Geophysics Section, Dublin Institute for Advanced Studies, Dublin, Ireland;; School of Geophysics, China University of Geosciences Beijing, Beijing, China;; School of Geophysics, China University of Geosciences Beijing, Beijing, China;; Department of Physics, University of Alberta, Edmonton, AB, Canada;; School of Geophysics, China University of Geosciences Beijing, Beijing, China;; School of Geophysics, China University of Geosciences Beijing, Beijing, China;; School of Geophysics, China University of Geosciences Beijing, Beijing, China;; School of Geophysics, China University of Geosciences Beijing, Beijing, China;; School of Geophysics, China University of Geosciences Beijing, Beijing, China;

Crustal weakening and transgressive melt penetrative intrusion across the Kunlun Shan inferred from INDEPTH Phase III and Phase IV magnetotelluric data

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