About This Item
- Full TextFull Text(subscription required)
- Pay-Per-View PurchasePay-Per-View
Purchase Options Explain
Share This Item
The AAPG/Datapages Combined Publications Database
Journal of Sedimentary Research (SEPM)
Abstract
Megapolygons in Ladinian Limestones of Triassic of Southern Alps: Evidence of Deformation by Penecontemporaneous Desiccation and Cementation
Riccardo L. Assereto, Christopher G. St. C. Kendall
ABSTRACT
Saucer-like structures (one to two m. in diameter when observed in cross-section) of dolomitized laminar fenestral intramicrite are interbedded with dense burrowed Ladinian micrite of the Esino Formation. This Triassic sedimentary sequence is interpreted as representing a subtidal and intertidal carbonate mud flat capped by a supratidal flat of laminar fenestrate carbonate. This fenestral horizon shows evidence of early cementation, dolomitization, fracturing, upward folding and some overthrusting. A later subtidal carbonate mud fills the fractures and covers them. Similar deformation of bedding occurs in the Holocene subtidal intertidal, and supratidal sediments of the Persian Gulf off Qatar and Abu Dhabi, and in the supratidal sediments of Shark Bay, West Australia. The Ladinian pol gons of fenestrate sediment are interpreted to be the result of either desiccation contraction, or cementation expansion or more probably a combination of both.
Pay-Per-View Purchase Options
The article is available through a document delivery service. Explain these Purchase Options.
Watermarked PDF Document: $14 | |
Open PDF Document: $24 |