Deep fluids are important for the evolution and properties of the lower continental and arc
crust in tectonically active settings. They comprise four components: H2O, nonpolar gases …

As an important part of the Mediterranean-Himalayas geothermal belt, southern Tibet and
western Yunnan are the regions of China where high-temperature hydrothermal systems are …

Topography extracted from swath profiles along the northern, southern, and eastern margins
of the Tibetan Plateau show two end-member morphologies: steep, abrupt margins and long …

Shear-coupled teleseismic P waves sampling the interior of the Tibetan plateau provide
evidence of systematic variations in crustal structure. The crust thins by up to 20 km from …

We have developed a novel goal-oriented adaptive mesh refinement approach for finite-
element methods to model plane wave electromagnetic (EM) fields in 3-D earth models …

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 …

Ultrahigh-pressure (UHP) rocks in the NW Himalaya are some of the youngest on Earth, and
allow testing of critical questions of UHP formation and exhumation and the timing of the …

There are currently three types of algorithms in use for regularized 2-D inversion of
magnetotelluric (MT) data. All seek to minimize some functional which penalizes data misfit …

This article explores municipal acceptance of wind power in Sweden and draws conclusions
on the basis of semi-structured interviews with municipal decision-makers, together with …

Fifteen seismic stations were operated with about 20‐km spacing in southern Tibet across
the Zangbo suture (the collision zone between India and Asia) between May and October …