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transitional crust造句

"transitional crust"是什么意思   

例句與造句

  1. The earthquake occurred in the transition zone from the continental margin to the continent-ocean transitional crust.
  2. NVPM are the result of rifting when a continent breaks up to form an ocean, producing transitional crust without volcanism.
  3. 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.
  4. 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.
  5. 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.
  6. It's difficult to find transitional crust in a sentence. 用transitional crust造句挺難的
  7. 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.
  8. 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.
  9. 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.
  10. 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.
  11. 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.
  12. 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.

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