B。解析:板块边界主要有三种类型,分别是汇聚型边界(Convergent boundary)、离散型边界(Divergent boundary)和转换型边界(Transform boundary)。在离散型边界处板块相互分离,例如大洋中脊就是典型的离散型边界,那里新的地壳不断形成。而汇聚型边界是板块相互挤压碰撞的地方,转换型边界是板块相互滑动的地方,所以这题选B。
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It is during the past 300 Myr since supercontinent Pangaea and its breakup when palaeogeography is most accurately known that TPW events are most keenly testable. The Mesozoic Era appears to have potentially been an active time interval for TPW, but large uncertainties remain. According to ...
Tectonic Plates The crust lies on top of the mantle, a configuration that is stable because the upper mantle is made of peridotite and so is significantlymore densethan thecrust. Theboundary betweenthe crust and mantle is conventionally placed at theMohorovičić discontinuity, a boundary defined...
Taking Weihe Fault as a boundary, the area to the south is Qinling piedmont geothermal water system, which is mainly recharged by meteoric water and surface water of Qinling Mountains, while the area to the north is piedmont geothermal water system of North Mountains, which is mainly recharged ...
Active deformation in the Zagros-Makran transition zone inferred from GPS measurements in the interval 2000-2002 The actual N-S convergence between the Arabian and the Eurasian plates is partly accommodated in Iran along the Zagros fold and thrust belt with a shortening of 8 mm/yr in the centr...
a maximum depth of more than 26,000 feet. The trench is deepest from its western end to its midpoint, while it becomes shallower as it extends eastward. This is because toward its eastern end, the convergent boundary becomes a transform boundary, with the Pacific and North American plates ...
This basin is characterised by a thick siliciclastic or calcareous turbidite sequence and pelagic deposits formed from Albian to the early Eocene. The opening period ended with the convergence between the Iberian and Eurasian plates that inverted the Cantabrian-Pyrenean rift system and led to the ...
Compilation of maps and cross-sections is based on combined field and geophysical data. Full size image As part of this study, we investigated an area along the Ida Fault42 at the boundary between the Youanmi Terrane and the EGST, in the central Yilgarn Craton (Fig. 1). The two terra...