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This work reconstructs the evolution of a source-to-sink system in a transpressional setting from compositional changes within its deep-water clastic offshoots. Field-based clast counts on 10 conglomerate beds of three transects, combined with petrog
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::67ca167c03def32c8a26f6676b0e63e3
https://hdl.handle.net/11383/2142052
https://hdl.handle.net/11383/2142052