Chinese–English

走向滑动断层

zǒu xiàng huá dòng duàn céng · zou xiang hua dong duan ceng

Traditional 走向滑動斷層

Meaning

CC-CEDICT

strike-slip fault (geology)
fault line where the two sides slide horizontally past one another

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Definitions adapted from CC-CEDICT, published by MDBG and its contributors, under CC BY-SA 4.0. Pinyin display and entry grouping have been adapted.

Meaning

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