The paleoenvironmental distribution of Phanerozoic wrinkle structures
Abstract
null null Wrinkle structures are microbially induced sedimentary structures that are known to have formed in ancient marine siliciclastic environments. This study reviews the sedimentary context and paleoenvironmental distribution of these sedimentary structures throughout three distinct intervals of the Phanerozoic: the Cambrian, the post-Cambrian Paleozoic, and the Lower Triassic. During these times, wrinkle structures are found primarily...
Paper Details
Title
The paleoenvironmental distribution of Phanerozoic wrinkle structures
Published Date
Oct 1, 2009
Journal
Volume
96
Issue
3
Pages
181 - 195
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