transitional crust造句
例句與造句
- The earthquake occurred in the transition zone from the continental margin to the continent-ocean transitional crust.
- NVPM are the result of rifting when a continent breaks up to form an ocean, producing transitional crust without volcanism.
- The continental crust forms a stable Mesoproterozoic craton which changes across a broad continental margin and transitional crust into true oceanic crust of the Gulf of Mexico.
- While the Gulf of Mexico was a restricted basin, the subsiding transitional crust was blanketed by the widespread deposition of Louann Salt and associated anhydrite evaporites.
- Further basinwards, the transitional crust is replaced by the oceanic crust characterized by a prominent gravity high and a well-imaged Moho reflection on seismic lines.
- It's difficult to find transitional crust in a sentence. 用transitional crust造句挺難的
- The first describes the relationship between rift orientation and plate motion, the second describes the nature of transitional crust, and the third describes post-rift sedimentation.
- These evaporites overlay a thick transitional crust, the local basement rock prior to rifting, and deposition of salts continued over the forming oceanic crust as rifting spread the sea floor throughout the Jurassic.
- Transitional crust occurs on the slope in water depths of 1500 3000 m and is characterized by a prominent gravity low and a northeast-southwest-trending chain of seamounts of Late Cretaceous-Paleocene age.
- This thinning created a broad zone of thick transitional crust, which displays modest and uneven thinning with block faulting, and a broad zone of uniformly thinned transitional crust, which is half the typical thickness, 35 kilometers, of normal continental crust.
- This thinning created a broad zone of thick transitional crust, which displays modest and uneven thinning with block faulting, and a broad zone of uniformly thinned transitional crust, which is half the typical thickness, 35 kilometers, of normal continental crust.
- In fact, passive margins are extremely long, and vary along their length in rift geometry, nature of transitional crust, and sediment supply; it is more appropriate to subdivide individual passive margins into segments on this basis and apply the threefold classification to each segment.