中国大陆边缘和西太平洋洋壳之间的黄海海域，属于过渡型地壳结构。
Yellow Sea area, located between the margin of China's mainland and the oceanic crust of the Western Pacific ocean, has transitional crustal structure.
南海是东亚大陆边缘的巨型陆缘海，属大陆—大洋过渡型地壳构造区。
The South China Sea is a huge marginal sea at East-Asian continental margin, and a tectonic region of the transitional crust type from continental to oceanic.
中国大陆边缘和西太平洋洋壳之间的黄海海域，属于过渡型地壳结构。
Yellow Sea area, located between the margin of China's mainland and the oceanic crust of...
它是分布于过渡性地壳上的、由起源于下地壳—上地幔的过渡性岩浆的衍生物形成的斑岩型铜银锡矿床。
It is a porphyry copper-silver-tin deposit that occurs in the transitional crust and was formed by derivatives of the lower crustal-upper mantle transitional magma.
它是分布于过渡性地壳上的、由起源于下地壳—上地幔的过渡性岩浆的衍生物形成的斑岩型铜银锡矿床。
It is a porphyry copper-silver-tin deposit that occurs in the transitional crust and was formed by derivatives of the lower crustal-upper mantle transitional magma.
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