Geodetic data support a short-term continental deformation localized in faults bounding
lithospheric blocks. Whether major “faults” observed at the surface affect the lithospheric …

The last 20 years has seen a dramatic improvement in the quantity and quality of geodetic
measurements of the earthquake loading cycle. In this paper we compile and review these …

It is well recognized that active arc volcanism at nearly all subduction zones requires
temperatures greater than 1200° C in the subarc mantle, despite the underthrusting cool …

We present new geodetic results of crustal velocities over a large part of northern Asia
based on GPS measurements in the Baikal rift zone and Mongolia spanning the 1994–2002 …

To specify quantitatively the effect of pressure and water weakening on the flow strength of
feldspar we performed triaxial creep experiments in a gas deformation apparatus at …

During the first 2 years following the 2002 Mw= 7.9 Denali, Alaska, strike‐slip earthquake, a
large array of Global Positioning System (GPS) receivers recorded rapid postseismic surface …

The Tibetan Plateau is the type example of a large orogenic plateau formed as a result of
continent‐continent collision. The morphology of the plateau and its margins suggests that …

At subduction zones, geophysical and geochemical observations indicate that the arc and
backarc regions are hot, in spite of the cooling effects of a subducting plate. At the well …

Central Mongolia is a prominent region of intracontinental surface deformation and
intraplate volcanism. To study these processes, which are poorly understood, we collected …

Constraining magnitudes of mechanical and thermo-mechanical parameters of rocks and
shear zones are the important goals in structural geology and tectonics (Talbot in J Struct …