Resistive (dry?) lower crust in an active orogen, Nanga Parbat, northern Pakistan
- 1 January 2000
- journal article
- Published by Elsevier in Tectonophysics
- Vol. 316 (3-4) , 359-380
- https://doi.org/10.1016/s0040-1951(99)00264-4
Abstract
No abstract availableThis publication has 26 references indexed in Scilit:
- Geochemistry of a dry steam geothermal zone formed during rapid uplift of Nanga Parbat, northern PakistanChemical Geology, 1997
- Electrically Conductive Crust in Southern Tibet from INDEPTH Magnetotelluric SurveyingScience, 1996
- A three-dimensional magnetotelluric investigation of the California Basin and RangeJournal of Geophysical Research: Solid Earth, 1996
- Robust smooth magneto tell uric transfer functionsGeophysical Journal International, 1996
- Active hydrothermal systems during the recent uplift of Nanga Parbat, Pakistan HimalayaJournal of Geophysical Research, 1995
- Boiling fluids in a region of rapid uplift, Nanga Parbat Massif, PakistanEarth and Planetary Science Letters, 1994
- Three-dimensional magnetotelluric inversion using conjugate gradientsGeophysical Journal International, 1993
- Trapping of aqueous fluids in the deep crustGeophysical Research Letters, 1990
- Decomposition of magnetotelluric impedance tensors in the presence of local three‐dimensional galvanic distortionJournal of Geophysical Research, 1989
- On the robust estimation of power spectra, coherences, and transfer functionsJournal of Geophysical Research, 1987