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pro vyhledávání: '"Yuemeng Niu"'
Publikováno v:
Energy Geoscience, Vol 4, Iss 3, Pp 100148- (2023)
Transfer zones are structural areas of faults interactions where fault motion or displacement can be transferred from one fault to another, regional strain maintains laterally constant. Transfer zones are widely developed in rift basins and have sign
Externí odkaz:
https://doaj.org/article/8ad2ce5cc1d94128a426afd0822ef66c
