(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...
Main Authors: | , |
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Format: | Dataset |
Language: | English |
Published: |
PANGAEA
1978
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Subjects: | |
Online Access: | https://dx.doi.org/10.1594/pangaea.718122 https://doi.pangaea.de/10.1594/PANGAEA.718122 |
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. ... |
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