標(biāo)題: Titlebook: Geology of the Cayman Islands; Evolution of Complex Brian Jones Book 2022 The Editor(s) (if applicable) and The Author(s), under exclusive [打印本頁] 作者: DART 時(shí)間: 2025-3-21 17:09
書目名稱Geology of the Cayman Islands影響因子(影響力)
書目名稱Geology of the Cayman Islands影響因子(影響力)學(xué)科排名
書目名稱Geology of the Cayman Islands網(wǎng)絡(luò)公開度
書目名稱Geology of the Cayman Islands網(wǎng)絡(luò)公開度學(xué)科排名
書目名稱Geology of the Cayman Islands被引頻次
書目名稱Geology of the Cayman Islands被引頻次學(xué)科排名
書目名稱Geology of the Cayman Islands年度引用
書目名稱Geology of the Cayman Islands年度引用學(xué)科排名
書目名稱Geology of the Cayman Islands讀者反饋
書目名稱Geology of the Cayman Islands讀者反饋學(xué)科排名
作者: flourish 時(shí)間: 2025-3-21 23:20
https://doi.org/10.1007/978-3-031-30808-6The Cayman Islands, comprising Grand Cayman, Little Cayman, and Cayman Brac, are located in the central part of the Caribbean Sea.作者: committed 時(shí)間: 2025-3-22 02:17
Introduction,The Cayman Islands, comprising Grand Cayman, Little Cayman, and Cayman Brac, are located in the central part of the Caribbean Sea.作者: Allege 時(shí)間: 2025-3-22 05:35
Brian JonesBrings together 40 years worth of research on the Cayman Islands.An overview of the evolution of complex carbonate successions on Isolated Oceanic Islands.Provides a history of geological investigatio作者: 讓你明白 時(shí)間: 2025-3-22 09:42 作者: 侵蝕 時(shí)間: 2025-3-22 15:05 作者: 侵蝕 時(shí)間: 2025-3-22 21:07 作者: PAEAN 時(shí)間: 2025-3-22 21:32 作者: NUDGE 時(shí)間: 2025-3-23 01:24
https://doi.org/10.1007/978-3-319-56839-3 Brac, and Little Cayman. Although exposed successions are generally <5?m thick, subsurface sequences on the western peninsula of Grand Cayman are up to 21.5?m thick. The formation rests unconformably on the Cayman Formation and is unconformably overlain by the Ironshore Formation. In many areas, mu作者: IDEAS 時(shí)間: 2025-3-23 07:07 作者: 占卜者 時(shí)間: 2025-3-23 11:17 作者: Antarctic 時(shí)間: 2025-3-23 14:59
Aetiology and Epidemiology of Breast Cancers. The seaward margins of the marine shelves around each island are defined by the 20?m isobath, which is the edge of the drop-off into deep water. As a result, the shelves around the islands are generally no more than 500?m wide. Lagoons, formed where fringing reefs have grown from headland to head作者: AGONY 時(shí)間: 2025-3-23 20:10
https://doi.org/10.1007/978-981-15-2937-5dolostones of the Cayman Formation and Pedro Castle Formation, is characterized by dark grey to black phytokarst surfaces that are reflective of various types of microbes, including bacteria, fungi, and cyanobacteria, that actively sculpted the topographically complex phytokarst surfaces. Surface ka作者: prediabetes 時(shí)間: 2025-3-24 00:58 作者: 甜得發(fā)膩 時(shí)間: 2025-3-24 04:41 作者: 粗鄙的人 時(shí)間: 2025-3-24 08:36
Tectonic Setting of the Cayman Islands,eparated from the depths of the Cayman Trench by the Oriente Transform Fault. The Mid-Cayman Rise, which is an active spreading center, is located off the southwest corner of Grand Cayman. Grand Cayman commonly experiences earthquakes that are triggered by activity along the Oriente Transform Fault 作者: 雄辯 時(shí)間: 2025-3-24 11:54 作者: 屈尊 時(shí)間: 2025-3-24 17:51
,Bluff Group—The Cayman Formation, unconformities with significant karstic relief. Although the Cayman Formation is at least 150?m thick, its true original thickness is unknown because of the relief on these boundaries. This formation developed during the Middle Miocene when marine sediments were deposited on an open bank in waters 作者: 枯萎將要 時(shí)間: 2025-3-24 21:30
,Bluff Group—Pedro Castle Formation, Brac, and Little Cayman. Although exposed successions are generally <5?m thick, subsurface sequences on the western peninsula of Grand Cayman are up to 21.5?m thick. The formation rests unconformably on the Cayman Formation and is unconformably overlain by the Ironshore Formation. In many areas, mu作者: B-cell 時(shí)間: 2025-3-25 00:50 作者: 相互影響 時(shí)間: 2025-3-25 04:06
Ironshore Formation,stones in this formation are typically dark grey to black in colour due to microbially mediated weathering. On Grand Cayman, large areas of the formation are covered by mangrove peats. The formation comprises Units A, B, C, D, E, and F that formed during highstand conditions that existed ~400?ka, 34作者: 執(zhí) 時(shí)間: 2025-3-25 07:39
Modern Carbonate Environments,s. The seaward margins of the marine shelves around each island are defined by the 20?m isobath, which is the edge of the drop-off into deep water. As a result, the shelves around the islands are generally no more than 500?m wide. Lagoons, formed where fringing reefs have grown from headland to head作者: Mortar 時(shí)間: 2025-3-25 11:48
Karst on the Cayman Islands,dolostones of the Cayman Formation and Pedro Castle Formation, is characterized by dark grey to black phytokarst surfaces that are reflective of various types of microbes, including bacteria, fungi, and cyanobacteria, that actively sculpted the topographically complex phytokarst surfaces. Surface ka作者: 侵害 時(shí)間: 2025-3-25 17:07 作者: IDEAS 時(shí)間: 2025-3-25 20:24
Hydrogeology,he major one on Cayman Brac. Other smaller lenses are found at various locations on both islands. No freshwater lenses have been identified on Little Cayman. There are no surface rivers or streams on the Cayman Islands because rainwater rapidly flows into the subsurface via fractures and joints that作者: 憤世嫉俗者 時(shí)間: 2025-3-26 01:58 作者: 異教徒 時(shí)間: 2025-3-26 06:17 作者: 使迷惑 時(shí)間: 2025-3-26 09:44 作者: Atrium 時(shí)間: 2025-3-26 15:39 作者: armistice 時(shí)間: 2025-3-26 17:50
RTL Design of Registers and Memories,lostones (zoned euhedral crystals up to 1.5?mm long) that are characterized by numerous different diagenetic stages that included the development of limpid dolomite cements, calcite cements, and complex vadose cements formed of calcite and dolomite. The Brac Formation on Grand Cayman is poorly under作者: 懸崖 時(shí)間: 2025-3-26 23:48
Digital Logic Design Using Verilogare echinoids. There are, however, only scattered, small coral patch reefs. Fossil-mouldic porosity is common given that the aragonitic skeletons of the corals and other organisms were commonly lost during early diagenesis. The dolostones, characterized by high porosity (up to 48%), are commonly cut作者: 預(yù)知 時(shí)間: 2025-3-27 02:36
https://doi.org/10.1007/978-3-319-56839-3hytokarst surfaces on the Pedro Castle Formation are generally more subdued than those on the Cayman Formation because the limestones–dolostones are not as hard as those in the Cayman Formation. The dolostones are typically formed of anhedral to euhedral dolomite crystals that are mostly <50?μm long作者: Ingenuity 時(shí)間: 2025-3-27 05:52 作者: 藝術(shù) 時(shí)間: 2025-3-27 11:49 作者: 意見一致 時(shí)間: 2025-3-27 15:07 作者: 輕快來事 時(shí)間: 2025-3-27 19:42 作者: Ambulatory 時(shí)間: 2025-3-28 01:54
Introducing Online Brand Communities,the late 1800s. The phosphates that remain on Little Cayman are mostly formed of hydroxylapatite with boehmite and crandallite being present locally. These deposits, formed largely of P.O., CaO, Al.O., Fe.O., and MnO, are petrographically complex with various admixtures of lithoclasts, coated grains作者: vibrant 時(shí)間: 2025-3-28 03:59 作者: Inflammation 時(shí)間: 2025-3-28 10:05
no longer exist). Most samples have been fully documented petrographically and geochemically..Data from 120 wells that have been drilled to depths up to 245 m (most less than 125 m). Wells have been cored and/978-3-031-08232-0978-3-031-08230-6作者: lactic 時(shí)間: 2025-3-28 10:40
,Bluff Group—the Brac Formation,lostones (zoned euhedral crystals up to 1.5?mm long) that are characterized by numerous different diagenetic stages that included the development of limpid dolomite cements, calcite cements, and complex vadose cements formed of calcite and dolomite. The Brac Formation on Grand Cayman is poorly under作者: Vulvodynia 時(shí)間: 2025-3-28 18:18 作者: 能得到 時(shí)間: 2025-3-28 21:32 作者: 亂砍 時(shí)間: 2025-3-28 23:24 作者: 驚呼 時(shí)間: 2025-3-29 03:50 作者: Arresting 時(shí)間: 2025-3-29 09:47
Modern Carbonate Environments,oons. Although infrequent, storms and hurricanes have a major impact on these depositional systems by moving large amounts of sediment onshore or offshore from the lagoons and open shelves. The lagoons, characterized by a diverse array of facies, typically have extensive . banks in the quieter, near作者: monopoly 時(shí)間: 2025-3-29 12:08 作者: mercenary 時(shí)間: 2025-3-29 18:52
Terra Rossa, Phosphate, and Mangrove Swamps,the late 1800s. The phosphates that remain on Little Cayman are mostly formed of hydroxylapatite with boehmite and crandallite being present locally. These deposits, formed largely of P.O., CaO, Al.O., Fe.O., and MnO, are petrographically complex with various admixtures of lithoclasts, coated grains作者: 用樹皮 時(shí)間: 2025-3-29 19:58
Hydrogeology,mplex hydrogeology, and variable hydrological conditions. Water flow into and out of the lenses is largely controlled by the fractures in the karstic terrains that allow intrusion of seawater or saline water, enhance hydrodynamic dispersion, and define lens geometry. The porosity and permeability of作者: Obstreperous 時(shí)間: 2025-3-30 02:07
