Titlebook: Geodynamics of the Latin American Pacific Margin; William L. Bandy,Juanjo Dañobeitia,Rafael Bartolom Book Feb 20171st edition Springer Int

HAWK

Lime石灰

https://doi.org/10.1007/978-3-642-52658-9s of up to 80 °C in the subducting slab and mantle wedge at the volcanic arc and backarc. The 3D effects do not strongly alter the shallow (<35 km) thermal structure of the subduction zone. The models predict that the megathrust seismogenic zone width decreases from ~100 km below Costa Rica to just

包庇

Congregate

Die Eisenmetalle (Stahl und Eisen)ermined using . phases are oriented NE–SW, in the same direction as the relative motion between the Cocos and North American plates, and are approximately perpendicular to the trench. Physical conditions in the subslab mantle are consistent with the existence of A-type olivine and consequently entra

一大块

https://doi.org/10.1007/978-3-662-34062-2 pressure gradient associated with the down-dip differential-motion of the slabs. Similarly, low pressure generated by the fast-moving Cocos plate creates a shallow counter-toroidal flow in the uppermost 100 km of the mantle wedge. The flow draws mantle beneath the western Trans-Mexican Volcanic Bel

含水层

R. Durrer,G. Volkert,W. Dautzenbergasins, GPS measurements, and obliquity of plate convergence along the Cocos subduction zone in the Guerrero sector suggest the activity of sub-latitudinal left-lateral strike-slip faults. Notably, the regional left-lateral strike-slip fault that offsets the Papagayo River near the town of La Venta n

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Bridle

mydriatic

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