SHELLEY, DAVID (1971) Hypothesis to Explain the Preferred Orientations of Quartz and Calcite Produced During Syntectonic Recrystallization. Geological Society of America Bulletin, 82 (7) 1943 doi:10.1130/0016-7606(1971)82[1943:htetpo]2.0.co;2

Reference Type | Journal (article/letter/editorial) | ||
---|---|---|---|
Title | Hypothesis to Explain the Preferred Orientations of Quartz and Calcite Produced During Syntectonic Recrystallization | ||
Journal | Geological Society of America Bulletin | ||
Authors | SHELLEY, DAVID | Author | |
Year | 1971 | Volume | 82 |
Issue | 7 | ||
Publisher | Geological Society of America | ||
DOI | doi:10.1130/0016-7606(1971)82[1943:htetpo]2.0.co;2Search in ResearchGate | ||
Generate Citation Formats | |||
Mindat Ref. ID | 50898 | Long-form Identifier | mindat:1:5:50898:6 |
GUID | 0 | ||
Full Reference | SHELLEY, DAVID (1971) Hypothesis to Explain the Preferred Orientations of Quartz and Calcite Produced During Syntectonic Recrystallization. Geological Society of America Bulletin, 82 (7) 1943 doi:10.1130/0016-7606(1971)82[1943:htetpo]2.0.co;2 | ||
Plain Text | SHELLEY, DAVID (1971) Hypothesis to Explain the Preferred Orientations of Quartz and Calcite Produced During Syntectonic Recrystallization. Geological Society of America Bulletin, 82 (7) 1943 doi:10.1130/0016-7606(1971)82[1943:htetpo]2.0.co;2 | ||
In | (1971) Geological Society of America Bulletin Vol. 82 (7) Geological Society of America |
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