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Dear Colleagues,


we invite you  to submit an abstract to the following Session of the

GSA Cordilleran Section Annual Meeting 2013,
20-22 May 2013, Fresno, California (USA).
http://www.geosociety.org/Sections/cord/2013mtg/


Session T2 -
Mélanges: comparison and contrast between Circum Pacific and Tethyan chaotic rock bodies and modern submarine analogues
Conveners: Yildirim Dilek, Andrea Festa, and Yujiro Ogawa
http://www.geosociety.org/Sections/cord/2013mtg/techprog.htm


Deadline
for abstract submissions is 19 February 2013


Summary of the session:

Our current knowledge of mélanges and chaotic rock bodies has been derived to the largest extent from the U.S. Cordillera concept of mélanges and its comparison with the Circum-Pacific and Tethyan mélange occurrences. However, there are some major differences, as well as strong similarities, between the mélange-forming processes that have been documented from the Cordilleran and Tethyan orogenic systems. Mélange-forming processes in Tethyan-type orogenic belts are commonly associated with passive margin evolution, subduction, and obduction of oceanic lithosphere, continental collision, and intra-continental deformation. Mélanges in Cordilleran-type orogenic belts are commonly involved, on the other hand, in the dynamics and mechanical stability of accretionary wedges, and hence are mostly the products of offscraping, underplating, mass-transport movements (olistostromes), subduction channel dynamics (flow mélanges), and mud diapirism. This session will provide an international forum for the exchange of current ideas and information about mélanges and chaotic rock bodies from the Circum-Pacific and Tethyan case studies, across the disciplinary boundaries (e.g., stratigraphy, structural geology, tectonics, sedimentology, marine geology, geochemistry, and thermochronology). Contributions covering a large spectrum of geological and geodynamic environments both on land and in modern submarine settings, in which mélanges, other chaotic rock bodies, and mud diapirs/volcanoes develop are welcome.

Relevant Field Trips: F7: Mélanges, HP Metamorphism, Subduction Accretion and Erosion, Subduction Megathrusts and Ophiolites: The Franciscan and Related Rocks; F3: From Deep to Modern Time along the Western Sierra Nevada Foothills–San Joaquin to Kern Drainages.



Kind Regards,


The Session Conveners

Yildirim DILEK  (Miami University, USA)

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Andrea FESTA
(University of Torino, Italy)

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Yujiro OGAWA
(Century Tsukuba-Miraidaira, Japan)

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Andrea Festa
Dipartimento di Scienze della Terra
Universitŕ degli Studi di Torino
Via Valperga Caluso, 35
10125 - TORINO (Italy)
Phone: - +39-011-670.51.86
Fax: -+39-011-670.53.39
e-mail: [log in to unmask]
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