標(biāo)題: Titlebook: Carbonate Microfabrics; Richard Rezak (Professor Emeritus),Dawn L. Lavoie Book 1993 Springer-Verlag New York, Inc. 1993 chemistry.fabric.g [打印本頁] 作者: BULK 時間: 2025-3-21 17:38
書目名稱Carbonate Microfabrics影響因子(影響力)
作者: 熱心 時間: 2025-3-21 20:25
Carbonate Microfabrics Related to Subaerial Exposure and Paleosol Formationle, dune and beach sands display pronounced development of subaerial microfabric features. Pleistocene grainstones from San Salvador, Bahamas, contain rhizoliths, pedotubules, alveolar textures, calcified root hairs, Microcodium, laminated micrite, clotted micrite, soil pisoids, circumgranular crack作者: 詞匯 時間: 2025-3-22 03:41 作者: cumber 時間: 2025-3-22 07:40
Depositional and Early Diagenetic Controls on Texture and Fabric of Carbonate Mudbanks, South Florid texture and fabric. This is possible because, during the past two decades, the carbonate mudbanks of south Florida have been re-examined through a series of detailed stratigraphic studies (Wanless, 1976 and 1979; Warzeski, 1976; Enos and Perkins, 1979; Cottrell, 1989; Tagett, 1989; Wanless and Tage作者: Modify 時間: 2025-3-22 09:59 作者: 泥瓦匠 時間: 2025-3-22 15:19 作者: 泥瓦匠 時間: 2025-3-22 20:10
Cold-Seep Carbonates of the Louisiana Continental Slope-to-Basin Flooracts on Louisiana’s continental slope has led to the realization that authigenic carbonates are extremely abundant in locations where hydrocarbon seeps occur. These carbonates range from nodules formed in near-surface sediments, to massive reef-like buildups of yet unknown age that commonly have 20 作者: Nausea 時間: 2025-3-22 23:34
Habit of Bacterially Induced Precipitates of Calcium Carbonate: Examples from Laboratory Experimentsogists are recognizing the possibility that bacterially induced precipitates may form significant mineral deposits. Unfortunately, there are currently no criteria by which they can be recognized in Recent sediments, or in the rock record..Cultures of aerobic and facultative bacteria from cyanobacter作者: 有效 時間: 2025-3-23 02:59
Permeability Characteristics of Continental Slope and Deep-Water Carbonates from a Microfabric Perspverburden pressure. Most marine clays consist of smectites and illites that are fine-grained and platey. In contrast, carbonate sediments are composed of multishaped, multisized components. In general, clay-rich sediments consolidate to lower porosities and are less permeable than carbonates at give作者: foreign 時間: 2025-3-23 09:03
Microfabric and Physical Properties of Deep-Sea High Latitude Carbonate Oozesiceous ooze facies. These biogenous oozes are accumulations of the skeletons and skeletal fragments of calcareous and biosiliceous phytoplankton and zooplankton (nannofossils and foraminifers versus diatoms and radiolaria, respectively), which once lived in the upper water column. This “rain” of mic作者: nettle 時間: 2025-3-23 13:31
Preferred Orientation and Velocity Anisotropy in Marine Clay-Bearing Calcareous Sedimentss, ultrasonic .. and x-ray pole figure goniometry measurements were made on selected laminated calcareous claystones, laminated clay-bearing limestones, and nonlaminated limestones from various DSDP sites. Although all samples exhibit .. anisotropy (up to 20%), none exhibit calcite-preferred orienta作者: coalition 時間: 2025-3-23 17:30
Stress-Deformation Behavior of Two Carbonate Oozesained from the vicinity of the Christmas and Fanning Islands in the Pacific. Both sediments consisted of fine sand- to silt-sized carbonate foraminiferal and nannofossil oozes with 88 to 93% calcium carbonate. The samples had high water contents (89 to 127%), exhibited some plasticity, and were very作者: 土產(chǎn) 時間: 2025-3-23 20:50
Microfabric and Compositional Clues to Dominant Mud Mineralogy of Micrite Precursorsbric and composition in micrites may be related to the original mineralogy of the precursor lime mud. This chapter takes a broader look at Cenozoic (mainly Plio-Pleistocene) micritic limestones to evaluate the role of original mineralogy in the evolution of microfabric and composition in fine-graine作者: gorgeous 時間: 2025-3-24 00:12
Recrystallization of Dolomite with Timeicantly from those modern dolomites proposed as analogs for their genesis. Application of modern analogs to the origin of ancient dolomites all too often presumes that present-day fabrics and chemistries record conditions prevailing at the time of precipitation. Petrographic (plane-light and cathodo作者: forbid 時間: 2025-3-24 03:11 作者: 牲畜欄 時間: 2025-3-24 07:17
https://doi.org/10.1007/978-1-4684-9421-1chemistry; fabric; geochemistry; geology; geophysics作者: LITHE 時間: 2025-3-24 12:55
Springer-Verlag New York, Inc. 1993作者: recede 時間: 2025-3-24 15:40 作者: 無孔 時間: 2025-3-24 19:19
https://doi.org/10.1007/978-1-4612-1432-8g both light and electrons, can be said to define the modern era of microfabric studies. Since 1950 the attention of research workers has veered from one topic to another, qualifying old dogmas and embracing new ones, in a continual struggle to explain what the microscope reveals. The philosopher A.作者: 商談 時間: 2025-3-24 23:24
Three-Term Conjugate Gradient Methods,le, dune and beach sands display pronounced development of subaerial microfabric features. Pleistocene grainstones from San Salvador, Bahamas, contain rhizoliths, pedotubules, alveolar textures, calcified root hairs, Microcodium, laminated micrite, clotted micrite, soil pisoids, circumgranular crack作者: 啜泣 時間: 2025-3-25 05:04
Mathematical Analysis of Fluids in Motioneration of ooids. Channels are oriented perpendicular to the axis of highest ooid concentration and are linked to the transport system by their ebb-tidal deltas..On Joulters Cays, Bahamas, surface samples and cores from four channels provide information on trends of microfabrics that should be usefu作者: reserve 時間: 2025-3-25 09:59
Paolo Antonelli,Pierangelo Marcati texture and fabric. This is possible because, during the past two decades, the carbonate mudbanks of south Florida have been re-examined through a series of detailed stratigraphic studies (Wanless, 1976 and 1979; Warzeski, 1976; Enos and Perkins, 1979; Cottrell, 1989; Tagett, 1989; Wanless and Tage作者: evasive 時間: 2025-3-25 12:54
https://doi.org/10.1007/978-1-4419-9554-4structure and descends to a base level of accumulation in hollows and on ledges. In the inner recesses sediment settles out of suspension, and where it only partially fills cavities, geopetal fabrics are created. Once deep inside the structure the internal sediment is usually trapped in its final re作者: acrimony 時間: 2025-3-25 17:07
https://doi.org/10.1007/3-540-29264-0f fine-grained magnesian calcite. Most cementation occurs at slope depths within the permanent thermocline (200 to 800 m) and in areas of well-developed, long-slope currents..The overall effect of this process is to create muddy (micritic) lithologic units from originally mud-free sediments, thereby作者: 越自我 時間: 2025-3-25 23:31
Computational Fluid and Solid Mechanicsacts on Louisiana’s continental slope has led to the realization that authigenic carbonates are extremely abundant in locations where hydrocarbon seeps occur. These carbonates range from nodules formed in near-surface sediments, to massive reef-like buildups of yet unknown age that commonly have 20 作者: Statins 時間: 2025-3-26 02:30
Eduardo N. Dvorkin,Marcela B. Goldschmitogists are recognizing the possibility that bacterially induced precipitates may form significant mineral deposits. Unfortunately, there are currently no criteria by which they can be recognized in Recent sediments, or in the rock record..Cultures of aerobic and facultative bacteria from cyanobacter作者: 神圣在玷污 時間: 2025-3-26 05:37
https://doi.org/10.1007/3-540-29264-0verburden pressure. Most marine clays consist of smectites and illites that are fine-grained and platey. In contrast, carbonate sediments are composed of multishaped, multisized components. In general, clay-rich sediments consolidate to lower porosities and are less permeable than carbonates at give作者: 熟練 時間: 2025-3-26 08:55 作者: 忙碌 時間: 2025-3-26 14:50 作者: 蛛絲 時間: 2025-3-26 18:59 作者: uncertain 時間: 2025-3-26 23:08 作者: COKE 時間: 2025-3-27 02:09
Viscoelastic Continua at Large Deformations,icantly from those modern dolomites proposed as analogs for their genesis. Application of modern analogs to the origin of ancient dolomites all too often presumes that present-day fabrics and chemistries record conditions prevailing at the time of precipitation. Petrographic (plane-light and cathodo作者: 改革運(yùn)動 時間: 2025-3-27 06:12 作者: cauda-equina 時間: 2025-3-27 12:53 作者: Dappled 時間: 2025-3-27 16:58 作者: 方便 時間: 2025-3-27 21:33
Book 1993n the fields of geology, geophysics and geotechnique. This book, the result of a symposium and workshop on carbonate microfabrics, explores the relationship of microfabrics to fundamental properties and processes in carbonates. .Carbonate . .Microfabrics. will be of particular interest to geologists作者: 倔強(qiáng)一點(diǎn) 時間: 2025-3-27 23:36
Book 1993onship of microfabrics to fundamental properties and processes in carbonates. .Carbonate . .Microfabrics. will be of particular interest to geologists and is intended to be of general interest to researchers in such related fields as geochemistry, geophysics, and geotechnique.作者: glucagon 時間: 2025-3-28 02:10 作者: 失望昨天 時間: 2025-3-28 10:03 作者: myopia 時間: 2025-3-28 13:06 作者: 稱贊 時間: 2025-3-28 15:44
https://doi.org/10.1007/978-1-4612-1432-8our theories over the last few decades has become apparent as we have sought revelation in various diagenetic environments, first the meteoric, then the open-system marine, later the deep-burial and now the closed-system marine. The narrative of kaleidoscopic change points only to a similarly challe作者: 最高點(diǎn) 時間: 2025-3-28 19:23 作者: RENIN 時間: 2025-3-29 00:28 作者: LAIR 時間: 2025-3-29 04:52
https://doi.org/10.1007/978-1-4419-9554-4generations of internal sediments are created when sediment supply to cavities is in phases controlled by flushing of turbid water during storms, by framework fracturing, and bioerosion by framework-penetrating boring organisms. The main components of internal sediments of small cavities are silt-si作者: 賞錢 時間: 2025-3-29 08:33 作者: FLIP 時間: 2025-3-29 11:30 作者: 搜尋 時間: 2025-3-29 19:08 作者: CHIDE 時間: 2025-3-29 20:51 作者: flutter 時間: 2025-3-30 00:24 作者: cogitate 時間: 2025-3-30 07:04 作者: 使迷醉 時間: 2025-3-30 12:05 作者: 的’ 時間: 2025-3-30 14:10
Solid Mechanics and Its Applications of monomineralic allochems of known aragonite or HMC (high-magnesium calcite) mineralogy provide strong evidence supporting the inference of mineralogic control on the generation of ADP or CDP micrite microfabrics. The relationship between strontium contents and crystal size in micrites refutes int作者: 獸皮 時間: 2025-3-30 17:40 作者: 小丑 時間: 2025-3-30 21:40
https://doi.org/10.1007/978-3-662-04299-1d conglomerate from the Trenton Limestone. This indicates that the substrate has a large effect on the CSD. There is no simple nucleation and growth law that explains the CSD of most of the ancient dolomites studied. However, a qualitative model of continuous nucleation and flux-limited growth is co作者: Postulate 時間: 2025-3-31 02:04
Microfabrics in Carbonate Diagenesis: A Critical Look at Forty Years in Researchour theories over the last few decades has become apparent as we have sought revelation in various diagenetic environments, first the meteoric, then the open-system marine, later the deep-burial and now the closed-system marine. The narrative of kaleidoscopic change points only to a similarly challe作者: 陶器 時間: 2025-3-31 05:20
Trends of Sedimentary Microfabrics of Ooid Tidal Channels and Deltasannel, ooids are bimodal in size (large ooids have numerous laminae and small ooids have fewer laminae) and therefore less well sorted. Nuclei of ooids are dominated by peloids in all environments. A trend of increasing size of ooids on ebb-tidal deltas and along intervening beaches in the direction作者: Triglyceride 時間: 2025-3-31 10:24
Depositional and Early Diagenetic Controls on Texture and Fabric of Carbonate Mudbanks, South Florid south Florida have grown as physically dynamic sediment bodies and contain both physical and biogenic depositional facies. Mudbank facies are influenced to varying degrees by biological processes of sediment production, aggregation and substrate stabilization. Depositional facies have been partiall作者: Neutral-Spine 時間: 2025-3-31 16:24 作者: Hemiplegia 時間: 2025-3-31 21:24 作者: 主動 時間: 2025-3-31 23:43
