Sedimentary slope break belt was easy to be formed at the edge of platform and bio-herm or formed under differential compaction or transferred from fault slope break belt.

 
  • 沉積坡折帶則易在臺地和生物礁體的邊緣形成或由沉積的差異壓實(shí)作用和斷層坡折帶轉化而來(lái)。
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