標(biāo)題: Titlebook: Coated Grains; Tadeusz M. Peryt Conference proceedings 1983 Springer-Verlag Berlin Heidelberg 1983 Dolomite.Gestein.Karbonatgestein.Konkre [打印本頁(yè)] 作者: antibody 時(shí)間: 2025-3-21 16:24
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)公開度
書目名稱Coated Grains網(wǎng)絡(luò)公開度學(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
作者: 猛然一拉 時(shí)間: 2025-3-21 21:45 作者: extract 時(shí)間: 2025-3-22 00:47 作者: Flustered 時(shí)間: 2025-3-22 08:09
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作者: FIN 時(shí)間: 2025-3-22 09:04 作者: 好開玩笑 時(shí)間: 2025-3-22 15:45
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作者: 好開玩笑 時(shí)間: 2025-3-22 17:54
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作者: 使痛苦 時(shí)間: 2025-3-22 23:17
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作者: 犬儒主義者 時(shí)間: 2025-3-23 03:36
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作者: flamboyant 時(shí)間: 2025-3-23 05:39
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作者: 令人苦惱 時(shí)間: 2025-3-23 10:41
Martin Mullen,Marta Giralt,Liam Murray may be complex. The development of ooid shoals in the Bahamas has been examined by coring and seismic profiling by Ball (1967), Buchanan (1970), Hine (1977), Harris (1979), Palmer (1979) and Hine et al. (1981). The studies document facies, sedimentary structures, vertical sequences and geometry of 作者: 有惡意 時(shí)間: 2025-3-23 13:51 作者: Fissure 時(shí)間: 2025-3-23 22:05 作者: 豎琴 時(shí)間: 2025-3-24 00:37 作者: 正式通知 時(shí)間: 2025-3-24 03:32 作者: 遠(yuǎn)足 時(shí)間: 2025-3-24 09:51 作者: 簡(jiǎn)略 時(shí)間: 2025-3-24 13:44
https://doi.org/10.1057/9781137530981The Liassic carbonate platform in the Veneto is rich enough in oolitic rock-types to justify the fact that one of its components, an Upper Lias carbonate formation, is called the S. Vigilio Oolite.作者: 和平主義 時(shí)間: 2025-3-24 17:05 作者: Mettle 時(shí)間: 2025-3-24 22:39 作者: 陪審團(tuán)每個(gè)人 時(shí)間: 2025-3-25 00:37
Sedimentary Characteristics of Oolitic Carbonates from the Jialing-Jiang Formation [Lower Triassic (Sichuan Basin was an epicontinental sea in the late (Aurenig) of the Early Triassic. The sea was bounded to the north and west by land masses, and to the south by a submarine high, while to the east lay the open sea (Fig. 1). These paleogeographic features controlled sedimentation in the basin.作者: 必死 時(shí)間: 2025-3-25 03:23 作者: 飛鏢 時(shí)間: 2025-3-25 10:59 作者: angina-pectoris 時(shí)間: 2025-3-25 13:25 作者: 擁擠前 時(shí)間: 2025-3-25 16:10 作者: onlooker 時(shí)間: 2025-3-25 23:28 作者: geometrician 時(shí)間: 2025-3-26 02:50 作者: 有權(quán)威 時(shí)間: 2025-3-26 07:35
https://doi.org/10.1007/978-3-319-77134-2 These grains are classified according to their structure and environmental parameters (Peryt, this vol.). Peloids are micritic grains without recognizable structures and are represented by individual grains and aggregates. Ooids, oncoids, rhodoids, and vadoids are coated grains with distinct structural features.作者: Synchronism 時(shí)間: 2025-3-26 09:41 作者: Living-Will 時(shí)間: 2025-3-26 15:45 作者: dearth 時(shí)間: 2025-3-26 18:13
Looking to Brain Research for Insights,hamas (Illing 1954, Newell et al. 1960). This structure is normal for recent ooids from marine environments (for exceptions see Land et al. 1979). The μm-sized aragonite crystals are rod- or baton-shaped (Fabricius and Klingele 1970, Loreau 1970).作者: 用手捏 時(shí)間: 2025-3-27 00:33 作者: 綠州 時(shí)間: 2025-3-27 01:45 作者: 連詞 時(shí)間: 2025-3-27 07:46
https://doi.org/10.1007/978-3-319-77134-2of the eastern Swiss Alps which differed from an ooid in that the coated grain called oncoid possessed (Heim 1916, p. 566): (1) non-concentric overlapping of separate envelopes, (2) not exclusively rounded form, (3) compact structure, with or without nucleus, and (4) sharp or indistinct boundaries. 作者: 鋼盔 時(shí)間: 2025-3-27 12:50
Martin Mullen,Marta Giralt,Liam Murrayarine ooids, from Cayeux (1935) to Shearman et al. (1970) and has been reestablished by Simone (1974), Sandberg (1975) and Wilkinson and Landing (1978) only in the last ten years. (3) “Recrystallized structure” is developed in calcitized former aragonitic oolitic grains, in which “the larger irregul作者: 輕觸 時(shí)間: 2025-3-27 13:50 作者: 最低點(diǎn) 時(shí)間: 2025-3-27 18:20 作者: 逃避現(xiàn)實(shí) 時(shí)間: 2025-3-27 22:13
Conference proceedings 1983ed both to their intriguing form and their significance in facies inter- pretation and sedimentology and to their relevance to accumulations of hydrocarbons and other mineral deposits. This resulted in numerous publications on this subject, and the intention of this volume is to sum- marize the pres作者: sebaceous-gland 時(shí)間: 2025-3-28 04:04 作者: 打算 時(shí)間: 2025-3-28 06:29 作者: 束以馬具 時(shí)間: 2025-3-28 13:50 作者: 保存 時(shí)間: 2025-3-28 16:23 作者: 破裂 時(shí)間: 2025-3-28 22:44 作者: 高調(diào) 時(shí)間: 2025-3-29 02:00
as re- lated both to their intriguing form and their significance in facies inter- pretation and sedimentology and to their relevance to accumulations of hydrocarbons and other mineral deposits. This resulted in numerous publications on this subject, and the intention of this volume is to sum- mariz作者: 充足 時(shí)間: 2025-3-29 07:00 作者: 四海為家的人 時(shí)間: 2025-3-29 10:31 作者: epicardium 時(shí)間: 2025-3-29 15:10
Martin Mullen,Marta Giralt,Liam Murray (1977), Harris (1979), Palmer (1979) and Hine et al. (1981). The studies document facies, sedimentary structures, vertical sequences and geometry of bank-margin ooid accumulations. It is these sedimentary features that are critical in our interpretation of ancient oolite deposits seen in outcrop or borehole cores.作者: indoctrinate 時(shí)間: 2025-3-29 18:56
Activating the Brain in the Classroom,to locality, and therefore represent a small sample of compositions and fabrics possessed by coated grains. Although volumetrically insignificant, non-marine ooids from both high- and low-salinity systems are important in understanding the physical and chemical processes which give rise to variations in coated grains.作者: 屈尊 時(shí)間: 2025-3-29 23:48
Classification of Coated Grains: Discussions” of Richter and Besenecker (this vol.) and some of the ooids discussed by Richter (this vol.) — thermal ooids, cave ooids, aqueduct ooids, and power plant ooids — as vadoids, though this is not justified in my opinion. This was the reason for preparing the following comment.作者: Mitigate 時(shí)間: 2025-3-30 00:09 作者: preservative 時(shí)間: 2025-3-30 06:52
The Joulters Ooid Shoal, Great Bahama Bank (1977), Harris (1979), Palmer (1979) and Hine et al. (1981). The studies document facies, sedimentary structures, vertical sequences and geometry of bank-margin ooid accumulations. It is these sedimentary features that are critical in our interpretation of ancient oolite deposits seen in outcrop or borehole cores.作者: Instantaneous 時(shí)間: 2025-3-30 11:53 作者: Infantry 時(shí)間: 2025-3-30 15:41
Accretionary Lapilli in Volcanic Ash Falls: Physical Factors Governing Their Formationt as his uncle C. Plinius (the elder) who died during the eruption, probably from respirational problems, he might have discovered in the ash layers peculiar pellets frequently exhibiting concentric textures. Such bodies are now generally referred to as accretionary lapilli, in preference over terms as volcanic hailstones, mud balls, etc.作者: Interstellar 時(shí)間: 2025-3-30 20:04
Cortical Fabrics in Calcite and Aragonite Ooidstices was also variable (e.g., Kettenbrink and Manger 1971), although the initial magnesium content of ancient calcite ooids is undocumented and the relative abundance of aragonite versus calcite phases has not been constant throughout Phanerozoic time (e.g., MacKenzie and Pigott 1981).作者: LUCY 時(shí)間: 2025-3-30 21:32 作者: Coordinate 時(shí)間: 2025-3-31 03:32 作者: 沒有貧窮 時(shí)間: 2025-3-31 06:49
Relict Sand Bodies and Bedforms of the Northern Bahamas: Evidence of Extensive Early Holocene Sand Topography are no longer in equilibrium with the modern environment. This suggests that sand movement was more vigorous and pervasive earlier in the Holocene on the bank tops and margins than at present.作者: Strength 時(shí)間: 2025-3-31 11:01 作者: 小鹿 時(shí)間: 2025-3-31 15:26 作者: Urea508 時(shí)間: 2025-3-31 18:37 作者: 投射 時(shí)間: 2025-4-1 01:04
