Late Albian, Cenomanian and Turonian Natih Supersequence of Oman: Type section for Orbiton 7 (103.6–89.0 Ma) [PDF]
, 2010 Moujahed Al-Husseini
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Groundwater microflora of the Aptian-Cenomanian deposits at the Igolsko-Talovoe field in Tomsk Region [PDF]
, 1999 The authors have studied the microbiological composition of the groundwater of the Aptian-Cenomanian deposits in the territory of the Igolsko-Talovoe field in Tomsk Region. The detected diversity of the physiological groups of bacteria can be a corrosive
Forst, R. +3 more
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Cirripedes from the Cenomanian Chalk Marl of Cambridge.
Proceedings of the Zoological Society of London, 1913 (Uploaded by Plazi from the Biodiversity Heritage Library) No abstract provided.
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PROBLEMS OF WELLS OPERATION IN CENOMANIAN DEPOSITS
Oil and Gas Studies, 2016 It is shown that Upper Cenomanian deposits are considered among the main productive formations for development for gas production. These deposits are presented by poor cemented reservoirs. The problem of Cenomanian wells operation is said to be related with sand production and formation of sand plugs in the borehole which leads to the flow rate decline.
E. V. Panikarovski, V. V. Panikarovski
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Subsurface relationships of Albian-Cenomanian shallow marine to nonmarine topsets of the Nanushuk Formation, northwestern NPRA, northern Alaska [PDF]
, 2016 P. L. Decker, D. L. LePain
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Revision of Cenomanian-Turonian (Upper Cretaceous) gastropods from Egypt [PDF]
, 2011 Ayoub-Hannaa, Wagih +1 more
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Upper Cretaceous (Cenomanian–Turonian) bivalves from northern Jordan, Middle East
Revista Mexicana de Ciencias Geológicas, 2018 Twelve species of bivalves are described for the Upper Cretaceous Ajlun Group of northern Jordan. The specimens were collected in three localities of the Fuheis (?middle to late Cenomanian), Hummar (late Cenomanian), and Shuayb (early Turonian ...
María del Carmen Perrilliat +2 more
doaj
Biogeochemical effects of volcanic degassing on the oxygen-state of the oceans during the Cenomanian/Turonian Anoxic Event 2 [PDF]
, 2011 FINAL ID: PP11A-1769 Cretaceous anoxic events may have been triggered by massive volcanic CO2 degassing as large igneous provinces (LIPs) were emplaced on the seafloor.
Floegel, Sascha +6 more
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Palaezoogeography and Late Cenomanian foraminifera of Western Siberia [PDF]
, 2016 Vera M. Podobina
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