Your single point of reference for all your Geotechnical Inquiries
No reviews have been submitted for this Publication so far.
You must be registered in order to submit a review.
You must be registered in order to submit a review.
Share this Information:
|
|
|
MIDDLE CRUSTAL DUCTILE DEFORMATION PATTERNS IN SOUTHERN TIBET: INSIGHTS FROM VORTICITY STUDIES IN MABJA DOME (2010)
New detailed microscopic kinematic analyses, deformation temperature estimates, and vorticity analyses within mid-crustal rocks from Mabja Dome show a downward progression from mixedtop-N and top-S shear in chloritoid-zone rocks, through dominantly top-S shear in garnet- and kyanite-zone rocks, to solely top-S shear in staurolite-zone and deeper rocks.
Reference:
Journal of Structural Geology 32 (2010) 70-85
Journal of Structural Geology 32 (2010) 70-85
Organization:
Department of Geological Sciences, Central Washington University, Ellensburg, WA 98926, USA
Tibet
Department of Geological Sciences, Central Washington University, Ellensburg, WA 98926, USA
Tibet
User Rating:
You must be registered to vote.
