(Table 1) Distribution of smectite and silica in sediments adjacent to and within ash beds from DSDP Hole 19-192 ...

Total peak areas of 17-, 10-, and 7-A clay minerals are shown. Typical detrital terrigenous clay from North Pacific - Bering Sea area is about 80 to 125 cm**2. This parameter establishes that ash layers have little clay. For X-ray amorphous materials distinction between opaline silica (opal-A) and g...

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Bibliographic Details
Main Authors: Hein, James R, Scholl, David W
Format: Dataset
Language:English
Published: PANGAEA 1978
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.718122
https://doi.pangaea.de/10.1594/PANGAEA.718122
Description
Summary:Total peak areas of 17-, 10-, and 7-A clay minerals are shown. Typical detrital terrigenous clay from North Pacific - Bering Sea area is about 80 to 125 cm**2. This parameter establishes that ash layers have little clay. For X-ray amorphous materials distinction between opaline silica (opal-A) and glass is based on morphology of X-ray curves and on thin sections. ...