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pro vyhledávání: '"Gayle E. Plenderleith"'
Fault relay ramps are important sediment delivery points along rift margins and often provide persistent flow pathways in deepwater sedimentary basins. They form as tilted rock volumes between en-echelon fault segments, which become modified through
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::6739d2e67670423ec7e1ff6e22accc83
Hybrid event beds are texturally and compositionally-diverse deposits preserved within deepwater settings. They are deposited by flows exhibiting ‘mixed behaviour’, forming complex successions of sandstone and mudstone, which are often challengin
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::d215dc9548aff1599628414c0cfd6c5c