Speculations on the genesis of crinoidal limestones in the Tethyan Jurassic
Crinoidal limestones in the Tethyan Jurassic often occur capping reef or carbonate-platform successions, and these bioclastic deposits commonly exhibit a lensoid form. They may also occur in tectonic fissures or as turbidites in basinal sequences. Their age is commonly Liassic, though they may be yo...
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| Format: | Journal article |
| Language: | English |
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Springer-Verlag
1971
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