全新世以来，该断裂的肃北至阿克塞一段以粘滑为主，而东边的巴个峡至昌马大坝之间断裂的滑动方式则为蠕滑。
The fault has been mainly in stick slip from Subei to Arkesai, and in creep slip from Bage Valley to Changma Dam since Holocene Epoch.
全新世以来，该断裂的肃北至阿克塞一段以粘滑为主，而东边的巴个峡至昌马大坝之间断裂的滑动方式则为蠕滑。
The fault has been mainly in stick slip from Subei to Arkesai, and in creep slip from Bage Valley to Changma Dam since Holocene Epoch.
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