Anagram & Information om | Engelska ordet REEFAL

Exempel på hur man kan använda REEFAL i en mening

• Main gas productions zones are between Eocene- Oligocene deposits; Hamitabat (turbiditic sandstones), Ceylan (tuffs), Sogucak (reefal limestone), and Osmancik (deltaic sandstone) formations.
• Shales, anhydrite, halite and reefal limestones of the uppermost middle Miocene Belayim lie unconformably on the Kareem.
• Jangziceras sichuanense was found in the Middle Silurian (Telychian) Lojoping Formation in Sichuan and Guizhou Provinces associated with orthoderids such as Sichuanaceras and Neosichuanoceras and oncocerids such as Oocerina and Guangyuanoceras among other nautiloid genera in reefal environments.
• The upper and lower units consist mostly of reefal limestones with bryozoa, gastropods, corals, sponges, brachiopods, bivalves and rudists.
• Possible bioherms within the carbonaceous intercalations and the archeocyathid reefs in the Cadí Nappe point at shelf or shelf edge deposits with some incorporated reefal complexes.
• Two facies domains can be distinguished: a detrital domain in the east (Serie de la Marteille) and a reefal domain with single corals, occasional oysters and nerineids in the west (Serie de Cercles).
• The shallow reefal biomicrite and mud-supported oolitic and pelletoidal biosparite limestones preserve fossils dating back to the Paleogene period.
• The reefal limestone preserves bivalve, gastropod and coral fossils dating back to the Messinian to Zanclean period.
• At the Clessinsperre, the type locality for the underlying Steinalm Formation, intense dolomitization has altered the microfacies characteristics of the Wetterstein Carbonate platform – typical are fore-reef carbonates, later reefal and back-reefal carbonates topped by lagoonal carbonates, making the original features hardly visible.
• Dagot Limestone - reefal limestone, calcarenites, biosparites, minor calcareous volcanic conglomerate, particularly at the base and middle section.
• The lime mudstones, grainstones and limestones of the formation were deposited in lagoonal and reefal environments.
• In addition, shallow water calcarenites, conglomerates, coral debris, hemipelagic sediments, breccia, limestones, felsite, foraminiferal sand, pelagic ooze, reefal limestones and sediments have been recovered.
• Rock samples obtained from the seamounts have yielded basaltic cobbles, manganese crusts, reefal limestone and scoria, as well as foraminifera sand, hyaloclastite and palagonite.

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