Titlebook: Coated Grains; Tadeusz M. Peryt Conference proceedings 1983 Springer-Verlag Berlin Heidelberg 1983 Dolomite.Gestein.Karbonatgestein.Konkre

antibody

書目名稱Coated Grains影響因子(影響力)




書目名稱Coated Grains影響因子(影響力)學(xué)科排名




書目名稱Coated Grains網(wǎng)絡(luò)公開(kāi)度




書目名稱Coated Grains網(wǎng)絡(luò)公開(kāi)度學(xué)科排名




書目名稱Coated Grains被引頻次




書目名稱Coated Grains被引頻次學(xué)科排名




書目名稱Coated Grains年度引用




書目名稱Coated Grains年度引用學(xué)科排名




書目名稱Coated Grains讀者反饋




書目名稱Coated Grains讀者反饋學(xué)科排名

猛然一拉

extract

Flustered

John L. Plews,Kim Misfeldt,Feisal Kirumiraory of ancient carbonate rocks may be inferred by studying these compositions. The carbon and oxygen isotopes in carbonate minerals have both been used extensively in the studies of environment of deposition, diagenesis and burial history (Gross 1964, Land 1970, Tan and Hudson 1974, Weber et al. 197

FIN

好開(kāi)玩笑

https://doi.org/10.1007/978-3-319-77134-2nd smooth as the trunk of a tree which divides into branches at the top.” This is the description of the initial ash cloud of the eruption of Mount Vesuvius on August 24, 79 A. D. as given by C. Plinius (the younger) in a letter to the historian P.C. Tacitus. Had he shown the same scientific interes

好開(kāi)玩笑

Martin Mullen,Marta Giralt,Liam Murray-like grains, resembling the roe of a fish, each of which has usually a small fragment of sand as a nucleus, around which concentric layers of calcareous matter have accumulated.” Also Sorby’s detailed description of calcareous “oolitic grains” from 1879 is still modern. He distinguished between the

使痛苦

Martin Mullen,Marta Giralt,Liam Murrayth cherty and chert-poor iron formations are similar morphologically to Recent calcareous ooids (Markun and Randazzo 1980, Rohrlich 1974). Ferriferous oolitic layers are always concentric and do not display the pervasive radial structure that cuts across concentric layers in many ancient calcitic oo

犬儒主義者

Martin Mullen,Marta Giralt,Liam Murrayabric. Compositionally, modern ooids consist of low-magnesian calcite (0%–5% MgCO.), high-magnesian calcite (10%–18% MgCO.) and aragonite with more than one phase commonly occurring within an individual cortex (e.g, Land et al. 1979). The primary mineralogy of ancient (now low-magnesian calcite) cor

flamboyant

Martin Mullen,Marta Giralt,Liam Murraythe dominant processes determining the character of these platform edges and distal lagoons (Hubbard et al. 1976, Hine 1977, Hine and Neumann 1977, Harris 1979, Palmer 1979, Hine et al. 1981a, b, Wilber 1981). The recent acquisition and analysis of high quality space and aerial imagery (see acknowle