Pyrrhotite remagnetizations in the Himalaya: a review

E Appel, C Crouzet, E Schill - Geological Society, London, Special …, 2012 - lyellcollection.org
This paper reviews results on the nature and thermo-tectonic interpretation of widespread
pyrrhotite remagnetizations in the Himalaya. Throughout the last two decades a large …

Miocene to recent exhumation of the central Himalaya determined from combined detrital zircon fission‐track and U/Pb analysis of Siwalik sediments, western Nepal

M Bernet, P van der Beek, R Pik, P Huyghe… - Basin …, 2006 - earthdoc.org
Fission‐track (FT) analysis of detrital zircon from synorogenic sediment is a well‐established
tool to examine the cooling and exhumation history of convergent mountain belts, but has so …

Preorogenic folds and syn‐orogenic basement tilts in an inverted hyperextended margin: The Northern Pyrenees case study

E Izquierdo‐Llavall, A Menant, C Aubourg, JP Callot… - …, 2020 - Wiley Online Library
The Chaînons Béarnais (CB, North Pyrenean Zone) resulted from the Cenozoic
contractional reactivation of the salt tectonics‐bearing, hyperextended margin that initiated …

Remagnetization of carbonate rocks in southern Tibet: Perspectives from rock magnetic and petrographic investigations

W Huang, PC Lippert, Y Zhang… - Journal of …, 2017 - Wiley Online Library
The latitudinal motion of the Tibetan Himalaya—the northernmost continental unit of the
Indian plate—is a key component in testing paleogeographic reconstructions of the Indian …

Tectono-metamorphic evolution of the Tethyan sedimentary sequence (Himalayas, SE Tibet)

C Montomoli, S Iaccarino, B Antolin… - Italian Journal of …, 2017 - pubs.geoscienceworld.org
Abstract The Tethyan Sedimentary Sequence, one of the major tectonic units of the
Himalayan belt crop** out in the inner portion of the chain, has been investigated in SE …

Pre-Miocene deformation of the Himalayan superstructure, Hidden valley, central Nepal

DA Kellett, L Godin - Journal of the Geological Society, 2009 - lyellcollection.org
Throughout the Himalaya, the Tethyan sedimentary sequence forms the detached carapace,
or superstructure, to exhumed mid-crustal rocks. In central Nepal, low metamorphic-grade …

Quantitative constraint on footwall rotations at the 15° 45′ N oceanic core complex, Mid‐Atlantic Ridge: Implications for oceanic detachment fault processes

CJ MacLeod, J Carlut, J Escartín… - Geochemistry …, 2011 - Wiley Online Library
The subsurface geometry of detachment faults at slow spreading mid‐ocean ridges is
debated: are they planar features that form and slip at low angles, as often inferred for their …

Temperature and age constraints on the metamorphism of the Tethyan Himalaya in Central Nepal: A multidisciplinary approach

C Crouzet, I Dunkl, L Paudel, P Arkai, TM Rainer… - Journal of Asian Earth …, 2007 - Elsevier
Metasediments of Devonian to Triassic age of the Tethyan Himalaya (TH) from several areas
in central and western Nepal, between western Dolpo and Marsyandi Valley, were sampled …

Kinematic evolution of the eastern Tethyan Himalaya: constraints from magnetic fabric and structural properties of the Triassic flysch in SE Tibet

B Antolín, E Appel, C Montomoli, I Dunkl… - Geological Society …, 2011 - lyellcollection.org
Anisotropy of magnetic susceptibility (AMS) combined with structural analysis are used in
this work with the aim to characterize the tectonic evolution of the Triassic flysch within the …

Experimental evaluation of magnetic interaction in pyrrhotite bearing samples

F Wehland, A Stancu, P Rochette, MJ Dekkers… - Physics of the Earth and …, 2005 - Elsevier
Pyrrhotite bearing metamorphic limestones have recently experienced an increasing
relevance in paleomagnetic research. Simple univectorial remanences document the …