(Table 1) Detrital modes for sand grains in sediment core CRP-2/2A

Dynamic provenance variations are deduced from sand-grain detrital modes in samples obtained from the CRP-2/2A drillcore. Below an important unconformity at 307 metres below sea floor (mbsf), sand grains in most of the sequence were dominantly derived from Beacon sandstone and Ferra dolerite sources...

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Bibliographic Details
Main Author: Smellie, John L
Format: Dataset
Language:English
Published: PANGAEA 2000
Subjects:
CRP
CWS
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.191104
https://doi.org/10.1594/PANGAEA.191104