P Xypolias - Journal of structural Geology, 2010 - Elsevier
Quantitative vorticity analyses in naturally deformed rocks are essential for studying the kinematics of flow in shear zones and can be performed using a range of methods, which …
L Godin, D Grujic, RD Law… - Geological Society, London …, 2006 - lyellcollection.org
The channel flow model aims to explain features common to metamorphic hinterlands of some collisional orogens, notably along the Himalaya-Tibet system. Channel flow describes …
Despite being the largest active collisional orogen on Earth, the growth mechanism of the Himalaya remains uncertain. Current debate has focused on the role of dynamic interaction …
A correlation has previously been noted between extremely high-uranium concentrations in zircon and apparent U/Pb age as measured in ion microprobe analysis. Here we present …
The presence of hot, weak crust is a central component of recent hypotheses that seek to explain the evolution of continent-continent collisions, and in particular may play an …
The largest crystalline unit representing the mid-crust in the Himalayan belt is the Greater Himalayan Sequence (GHS) which stretches all over the 2400 km of length of the belt. The …
D Grujic, CJ Warren, JL Wooden - Lithosphere, 2011 - pubs.geoscienceworld.org
Rare granulitized eclogites exposed in the eastern Himalaya provide insight into conditions and processes deep within the orogen. Sensitive high-resolution ion microprobe (SHRIMP) …
A high‐temperature shear zone, Toijem shear zone, with a top‐to‐the‐SW sense of shear affects the core of the Higher Himalayan Crystallines (HHC) in western Nepal. The shear …