摘要
中国和马来西亚Sarawak的Mulu喀斯特区发育的大型洞穴厅堂和天坑都与小洞道有关。它们主要沿破碎带发育,有些沿潜流带发育,其岩块崩塌并非仅与渗流排水有关。
In the karsts of China and Malaysian Sarawak large chambers and tiankengs are associated with much smaller cave passages. They have developed mainly on fracture zones, some within the phreas, where rock collapse is not associated only with vadose drainage.
出处
《中国岩溶》
CAS
CSCD
北大核心
2006年第B08期43-45,共3页
Carsologica Sinica
关键词
崩塌
断裂
大厅
落水洞
天坑
Collapse
Fracture
Chamber
Aven
Tiankeng
