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

開始沒有

https://doi.org/10.1007/978-3-642-52658-9uake seismogenic zone and volcanic arc magmatism. Here, we present the first three-dimensional (3D), steady-state kinematic-dynamic thermal model for the Costa Rica-Nicaragua subduction zone. The model consists of the subducting Cocos plate, the overriding Caribbean Plate, and a viscous mantle wedge

Canyon

https://doi.org/10.1007/978-3-642-86315-8nes and is therefore a natural laboratory for the analysis of curved orogens. The analysis of curved fold-and-thrust belts is a challenge because of the varying structural orientations within the belt. Based on seismic reflection lines, we created a 3-D subsurface model containing three major thrust

分離

https://doi.org/10.1007/978-3-642-52656-5cognized tectonic features at upper to mid-crustal depths. Our results support the hypotheses that the upper crust of the Oaxaca terrane is a residual?~20?km thick crust composed by an?~10?km thick faulted crustal upper layer and an?~10?km thick hydrated and/or mineralized layer. Oaxaca basement ove

Chipmunk

Die Eisenmetalle (Stahl und Eisen)rn Mexico starting at the coast of the Pacific Ocean and running north toward the Gulf of Mexico. In this segment of the Middle America Trench the oceanic Cocos plate subducts under the continental North American plate. The active volcanic arc is located at the southern end of the Trans-Mexican Volc

LEERY

Lyme-disease

R. Durrer,G. Volkert,W. Dautzenbergiated with the occurrence of subduction earthquakes and shallow earthquakes of the overriding plate. We present the results of geomorphic, structural, and fault kinematic analyses conducted on the convergent margin between the Cocos plate and the forearc region of the overriding North American plate

碎石

Zur Morphologie des Sittlichen,failure stress changes for the six major slow slip events (SSEs) that occurred below Mexico between late 2005 and mid-2011. Slip distributions are the first to be estimated from all continuous GPS data in central and southern Mexico, which better resolves slow slip in space and time than was previou

終端

Encephalitis

通便

978-3-319-51528-1Springer International Publishing AG 2017