標(biāo)題: Titlebook: Archean Rare-Metal Pegmatites in Zimbabwe and Western Australia; Geology and Metallog Thomas Dittrich,Thomas Seifert,J?rg Pf?nder Book 2019 [打印本頁(yè)] 作者: hector 時(shí)間: 2025-3-21 19:00
書目名稱Archean Rare-Metal Pegmatites in Zimbabwe and Western Australia影響因子(影響力)
書目名稱Archean Rare-Metal Pegmatites in Zimbabwe and Western Australia影響因子(影響力)學(xué)科排名
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書目名稱Archean Rare-Metal Pegmatites in Zimbabwe and Western Australia網(wǎng)絡(luò)公開度學(xué)科排名
書目名稱Archean Rare-Metal Pegmatites in Zimbabwe and Western Australia被引頻次
書目名稱Archean Rare-Metal Pegmatites in Zimbabwe and Western Australia被引頻次學(xué)科排名
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書目名稱Archean Rare-Metal Pegmatites in Zimbabwe and Western Australia讀者反饋
書目名稱Archean Rare-Metal Pegmatites in Zimbabwe and Western Australia讀者反饋學(xué)科排名
作者: 頑固 時(shí)間: 2025-3-21 23:16 作者: 編輯才信任 時(shí)間: 2025-3-22 02:11 作者: 思想靈活 時(shí)間: 2025-3-22 08:24
Geochemistry of LCT Pegmatites,the massive pollucite mineralisation. The geochemical study was also designed for potential prediction if a pegmatite potentially might host a yet not recognised massive pollucite mineralisation. Following these goals, the data from the pollucite-bearing Bikita pegmatite field are used for character作者: 顯微鏡 時(shí)間: 2025-3-22 12:13
Geochronology of Archean LCT Pegmatites,anco, Greenbushes, Bikita, Wodgina) were formed in relative narrow time intervals within the earth history. In addition, the temporal and spatial relation-ships of the pegmatites to potential source granites, their crystallisation history and geotectonic settings are still under debate. For the eval作者: Commodious 時(shí)間: 2025-3-22 13:27 作者: 斗志 時(shí)間: 2025-3-22 20:06 作者: GNAW 時(shí)間: 2025-3-22 23:35 作者: accessory 時(shí)間: 2025-3-23 03:55 作者: OCTO 時(shí)間: 2025-3-23 08:57 作者: facilitate 時(shí)間: 2025-3-23 10:20 作者: 嫻熟 時(shí)間: 2025-3-23 16:54 作者: labile 時(shí)間: 2025-3-23 19:06
Matthew R. Sanders,John A. Pickeringineralisation as at Bikita. The pegmatites of Bikita are hosted by metabasalts and metadiorites of the Upper Bulawayan Group in the Masvingo greenstone belt in the SE part of the Zimbabwe Craton. At about 2670 Ma the southern part of this craton was affected by deformation and up to granulite-facies作者: mendacity 時(shí)間: 2025-3-23 23:35 作者: 露天歷史劇 時(shí)間: 2025-3-24 06:23
Trauma-Focused Cognitive-Behavioral Therapythe massive pollucite mineralisation. The geochemical study was also designed for potential prediction if a pegmatite potentially might host a yet not recognised massive pollucite mineralisation. Following these goals, the data from the pollucite-bearing Bikita pegmatite field are used for character作者: 粗語 時(shí)間: 2025-3-24 06:56 作者: 點(diǎn)燃 時(shí)間: 2025-3-24 13:39 作者: forebear 時(shí)間: 2025-3-24 15:15 作者: 疼死我了 時(shí)間: 2025-3-24 19:20 作者: 善于騙人 時(shí)間: 2025-3-25 00:20
Book 2019ucite at Bikita (Zimbabwe Craton) and Tanco (Superior Province Craton) are of commercial importance. Common characteristics of world-class LCT pegmatite deposits include their Meso- to Neoarchean age and geological setting within greenstone belt lithologies on Archean Cratons..This study presents th作者: 暴露他抗議 時(shí)間: 2025-3-25 06:21
Trauma-Focused Cognitive-Behavioral Therapy by the mineral modes and assemblages gained by automated SEM-MLA (Mineral Liberation Analysis) from the same samples. The Geochemical investigations of the major and minor elements accentuates the solitary characteristics of the massive pollucite mineralisation at Bikita.作者: 冷淡一切 時(shí)間: 2025-3-25 10:04
Geochemistry of LCT Pegmatites, by the mineral modes and assemblages gained by automated SEM-MLA (Mineral Liberation Analysis) from the same samples. The Geochemical investigations of the major and minor elements accentuates the solitary characteristics of the massive pollucite mineralisation at Bikita.作者: 缺乏 時(shí)間: 2025-3-25 14:43 作者: PANIC 時(shí)間: 2025-3-25 19:34
Archean Rare-Metal Pegmatites in Zimbabwe and Western AustraliaGeology and Metallog作者: Infuriate 時(shí)間: 2025-3-26 00:03 作者: 分散 時(shí)間: 2025-3-26 03:20
Matthew R. Sanders,John A. Pickeringo the Southern Cross Terrane in the southeastern part of the craton. Two main contrasting models for the seven Archean geodynamic events (D0–D6) are discussed: modern-style plate tectonics with a westward directed subduction type scenario, or vertical crustal movements induced by constantly upwellin作者: Congeal 時(shí)間: 2025-3-26 06:39
Carolyn L. Webster-Stratton Ph.D., FAANte, spodumene and beryl. The samples were classified into 21 distinct mineral associations or pegmatite mineral zones. At Bikita, pollucite forms lens-like massive mineralisation with a crosscutting vein network of purple lepidolite, petalite, quartz and feldspar. Pollucite exhibits rather inhomogen作者: phase-2-enzyme 時(shí)間: 2025-3-26 10:56 作者: 1FAWN 時(shí)間: 2025-3-26 14:25 作者: 樂章 時(shí)間: 2025-3-26 17:39 作者: Apogee 時(shí)間: 2025-3-26 23:58 作者: 演繹 時(shí)間: 2025-3-27 01:59
Geological Settings of Archean Rare-Metal Pegmatites,o the Southern Cross Terrane in the southeastern part of the craton. Two main contrasting models for the seven Archean geodynamic events (D0–D6) are discussed: modern-style plate tectonics with a westward directed subduction type scenario, or vertical crustal movements induced by constantly upwellin作者: 未完成 時(shí)間: 2025-3-27 08:33
Petrography and Mineralogy,te, spodumene and beryl. The samples were classified into 21 distinct mineral associations or pegmatite mineral zones. At Bikita, pollucite forms lens-like massive mineralisation with a crosscutting vein network of purple lepidolite, petalite, quartz and feldspar. Pollucite exhibits rather inhomogen作者: APRON 時(shí)間: 2025-3-27 10:29
Geochronology of Archean LCT Pegmatites,e Neo-Archean pegmatites due to the widespread occurrence of these minerals as accessories in almost all samples. Furthermore, they are formed at a virtually constant level during pegmatite crystallisation from main crystallisation to late state hydrothermal overprint. The .Ar/.Ar ages cover a large作者: 珊瑚 時(shí)間: 2025-3-27 16:09 作者: Oafishness 時(shí)間: 2025-3-27 21:36 作者: 接觸 時(shí)間: 2025-3-28 01:25 作者: ALTER 時(shí)間: 2025-3-28 02:11
Book 2019 the complex geological framework: 1) enhances our knowledge of the formation ofLCT pegmatite systems, and 2) will contribute to the further exploration of additional world-class LCT pegmatite deposits, which 3) may host massive pollucite mineralisations.?.