نتایج جستجو برای: continent collision
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Article history: Creeping crustal faults often Received 2 February 2007 Received in revised form 11 September 2008 Accepted 22 September 2008 Available online xxxx Editor: R.D. van der Hilst
Abstract The Indian collision has deformed the eastern Asian continent in a multifaceted way, uplifting Tibet and surrounding mountains, activating ≥1,000 km‐long strike‐slip faults, opening Tertiary rifts oceanic basins up to ≈3,000 km away from Himalayas. Modeling such broad‐scale tectonics been challenging. While continent‐scale, lithospheric deformation appears have primarily taken‐up by lo...
Deformation pattern of the northeastern part of the Iranian-Arabian collision zone (i.e., mainly Sanandaj-Sirjan Belt or Zone) is the main concern of this paper. Here, we investigate the stress distribution and displacement pattern of Eghlid-Deh Bid area as affected by the position of Zagros suture using a three dimensional mechanical model. The modeled area is located between the Zagros Thrust...
Abstract We investigate how the mechanical properties of intra‐oceanic arcs affect collision style and associated stress‐strain evolution with buoyancy‐driven models subduction that accurately reproduce dynamic interaction lithosphere mantle. performed a series simulations only varying effective arc thickness as it controls buoyancy arcs. Our spontaneously evolve into two contrasting styles are...
New geochronological and geochemical data on magmatic activity from the India-Asia collision zone enables recognition of a distinct magmatic flare-up event that we ascribe to slab breakoff. This tie-point in the collisional record can be used to back-date to the time of initial impingement of the Indian continent with the Asian margin. Continental arc magmatism in southern Tibet during 80-40 Ma...
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