Titlebook: Reef Diagenesis; Johannes H. Schroeder,Bruce H. Purser Book 1986 Springer-Verlag Berlin Heidelberg 1986 Jura.Sediment.Trias.USA.biology.ca

Lactase

书目名称Reef Diagenesis影响因子(影响力)




书目名称Reef Diagenesis影响因子(影响力)学科排名




书目名称Reef Diagenesis网络公开度




书目名称Reef Diagenesis网络公开度学科排名




书目名称Reef Diagenesis被引频次




书目名称Reef Diagenesis被引频次学科排名




书目名称Reef Diagenesis年度引用




书目名称Reef Diagenesis年度引用学科排名




书目名称Reef Diagenesis读者反馈




书目名称Reef Diagenesis读者反馈学科排名

单调性

Regional Distribution of Submarine Cements Within an Epicontinental Reef System: Central Great Barri reefs throughout the world. This has led to the recognition that submarine cementation was an important process in many ancient reefs (e.g., Davies 1977, Lohman and Meyers 1977, James and Kobluk 1978, Mazzullo and Cys 1979, Walls et al. 1979, Mazzullo 1980, Playford 1980). The variety of synsedimen

sterilization

Model of Reef Diagenesis: Mururoa Atoll, French Polynesiacomposite nature of its volcanic basement (Gachon 1985) situated at minimum depths of 180 m below lagoonal sea level and at depths varying between 350 and 450 m below peripheral islands (Buigues 1982). Radiometric datings (Labeyrie et al. 1969) indicate that volcanic activity ceased about 7 million

发现

失误

plasma-cells

Diagenesis of a Miocene Reef-Platform: Jebel Abu Shaar, Gulf of Suez, Egypt on basement horsts and, when buried beneath evaporites, may be hydrocarbon reservoirs. The main structural features of the Gulf of Suez area consist of a series of tilted blocks related to the Neogene Rifting of the Red Sea and Gulf of Suez (Burollet et al. 1985). Two dominant fault trends, clysmic

脖子

陶瓷

Diagenesis of Mid-Cretaceous Rudist Reefs, Valles Platform, Mexicos of mid-Cretaceous rudist assemblages. These outcrops have long served as the most accessible depositional model (Kellum 1930, Muir 1936, Bonet 1952, Griffith et al. 1969), and, recently, as a diagenetic model (Aguayo 1978), for the spectacular oil-producing trend of the Golden Lane. Early submarin

拒绝

A Comparative Study of the Diagenesis in Diapir-Influenced Reef Atolls and a Fault Block Reef Platfosin is delineated by the Paleozoic massifs of the Cantabrian Mountains, to the east by the Pyrenees, and to the south by the Late Tertiary Ebro Basin. The tectonic history of the Vasco-Cantabrian ranges from the Triassic to the Tertiary but the major part of its fill (8000 m) is attributed to Late M

Comedienne

Micrite Diagenesis in Senonian Rudist Build-ups in Central Tunisiaing from marine cementation to freshwater dissolution and neomorphism. Many examples, not all of which are reefs, are compiled in two volumes on ., one edited by Bricker (1971), and the other by Schneidermann and Harris (1985). These diagenetic modifications have been recognized both in modern and a