“由于陆地形状的原因，整个系统变得非常，非常复杂，这让模拟印度洋上大气中的风向规律变化真的很有挑战性，”Han称。

"It has been really challenging to simulate atmospheric wind-pattern change over the Indian Ocean because the system is very, very complicated because of the land," han said.

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“由于陆地形状的原因，整个系统变得非常，非常复杂，这让模拟印度洋上大气中的风向规律变化真的很有挑战性，”Han 称。

“It has been really challenging to simulate atmospheric wind-pattern change over the Indian Ocean because the system is very, very complicated because of the land,” Han said.

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洋岛玄武岩以弄槐枕状熔岩为代表性火山岩，原为古特提斯洋盆中的夏威夷型洋岛，现保存在印支期前陆褶皱冲断带的一个外来岩席中。

The oceanic island basalt is represented by the Nonghuai pillow lava, which is, originally Hawaii type one in the Paleotethyan ocean, an allochthon in the Indosinian foreland fold and thrust belt.

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