Structural and Thermal Evolution of the Himalayan Thrust Belt in Midwestern Nepal 1-1-001-323-4330-323 and the sedimentary facies and

and the sedimentary facies and potential fluid pathways in the Shikoku Basin

and Joan Florsheim

detailed stratigraphy and paleontology of red beds of Late Triassic and Middle Jurassic age along the Gulf of Mexico coast region

John Roobol

contain geological

Structural and Thermal Evolution of the Himalayan Thrust Belt in Midwestern Nepal 1-1-001-323-4330-323 and the sedimentary facies andAuthors: P. G. DeCelles, B. Carrapa, T. P. Ojha, G. E. Gehrels, and D. Collins Spanning eight kilometers of topographic relief, the Himalayan fold thrust belt in Nepal has accommodated more than 700 km of Cenozoic convergence between the Indian subcontinent and Asia. Rapid tectonic shortening and erosion in a monsoonal climate have exhumed greenschist to upper amphibolite facies rocks along with unmetamorphosed rocks, including a 5 6 km thick Cenozoic