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

Lactase

書目名稱Reef Diagenesis影響因子(影響力)




書目名稱Reef Diagenesis影響因子(影響力)學(xué)科排名




書目名稱Reef Diagenesis網(wǎng)絡(luò)公開(kāi)度




書目名稱Reef Diagenesis網(wǎng)絡(luò)公開(kāi)度學(xué)科排名




書目名稱Reef Diagenesis被引頻次




書目名稱Reef Diagenesis被引頻次學(xué)科排名




書目名稱Reef Diagenesis年度引用




書目名稱Reef Diagenesis年度引用學(xué)科排名




書目名稱Reef Diagenesis讀者反饋




書目名稱Reef Diagenesis讀者反饋學(xué)科排名

單調(diào)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

發(fā)現(xiàn)

失誤

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

拒絕

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