Carbonate facies evolution from the late albian to Middle Cenomanian in Southern Istria (Croatia): influence of synsedimentary tectonics and extensive organic carbonate production

Josip Tišljar; Igor Vlahović; Ivo Velić; Dubravko Matičec; Julie Robson

doi:10.1007/bf02537361

Carbonate facies evolution from the late albian to Middle Cenomanian in Southern Istria (Croatia): influence of synsedimentary tectonics and extensive organic carbonate production

Facies ◽

10.1007/bf02537361 ◽

1998 ◽

Vol 38 (1) ◽

pp. 137-151 ◽

Cited By ~ 23

Author(s):

Josip Tišljar ◽

Igor Vlahović ◽

Ivo Velić ◽

Dubravko Matičec ◽

Julie Robson

Keyword(s):

Carbonate Facies ◽

Carbonate Production ◽

Synsedimentary Tectonics ◽

Organic Carbonate

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Zeolite-mediated production of cyclic organic carbonates: reaction of CO2 with styrene oxide on zeolite Y impregnated with metal halides

Reaction Chemistry & Engineering ◽

10.1039/d1re00036e ◽

2021 ◽

Vol 6 (4) ◽

pp. 672-678

Author(s):

Leonardo P. Ozorio ◽

Fábio J. S. Henrique ◽

James W. Comerford ◽

Michael North ◽

Claudio J. A. Mota

Keyword(s):

Zeolite Y ◽

Styrene Oxide ◽

Metal Halides ◽

Carbonate Production ◽

Organic Carbonates ◽

Organic Carbonate

Zeolites impregnated with metal halides as efficient catalysts for cyclic organic carbonate production.

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Prominent facies from the Lower/Middle Cambrian of the Dead Sea area (Jordan) and their palaeodepositional significance

BSGF - Earth Sciences Bulletin ◽

10.2113/173.6.547 ◽

2002 ◽

Vol 173 (6) ◽

pp. 547-552 ◽

Cited By ~ 9

Author(s):

Olaf Elicki ◽

Jörg Schneider ◽

Rafie Shinaq

Keyword(s):

High Energy ◽

Dead Sea ◽

Low Energy ◽

Carbonate Facies ◽

Carbonate Production ◽

Middle Cambrian ◽

The Dead ◽

Facies Types ◽

Sea Area ◽

Northern Jordan

Abstract New carbonate facies types are reported from the Cambrian Burj Fm. (Bilbilian) of the southern Dead Sea area (Jordan). They indicate the existence of a large low energy lagoon, with restricted water circulation and higher salinity, behind a high energy oolite shoal or shoal complex (back-barrier system). The transition between shoal and lagoon is marked by the interfingering of sediments from both environments, caused by washover events from the shoal into the lagoon behind. The lagoon itself was characterized by a low sedimentation rate and entire bioturbation. In a shoreward direction, the lagoonal facies changed into a microbial-dominated tidal or sabkha flat environment from which sediments were periodically reworked and redeposited into the lagoon. Comparison of our results with investigations of subsurface Cambrian deposits in southeastern and northern Jordan shows that lagoonal environments were the predominant carbonate production centres in this area during the short marine phase in the Cambrian of the Dead Sea area.

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