標(biāo)題: Titlebook: Geochemical Treasures and Petrogenetic Processes; John S. Armstrong-Altrin,Kailasa Pandarinath,Sanje Book 2022 The Editor(s) (if applicabl [打印本頁] 作者: NO610 時(shí)間: 2025-3-21 19:33
書目名稱Geochemical Treasures and Petrogenetic Processes影響因子(影響力)
書目名稱Geochemical Treasures and Petrogenetic Processes影響因子(影響力)學(xué)科排名
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書目名稱Geochemical Treasures and Petrogenetic Processes網(wǎng)絡(luò)公開度學(xué)科排名
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書目名稱Geochemical Treasures and Petrogenetic Processes年度引用學(xué)科排名
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書目名稱Geochemical Treasures and Petrogenetic Processes讀者反饋學(xué)科排名
作者: BORE 時(shí)間: 2025-3-22 00:12
Identification and Modeling of Hydrogeochemical Processes in an Arid Zone of Mexican Highlandsof groundwater. The infiltration of water enriched with CO. reacts with albite and K feldspar, releasing silica, Na., K., Mg., and HCO. and the formation of clays. Reverse modeling indicates the formation of calcite, hematite, alteration of magnetite, and dissolution of gypsum.作者: 組裝 時(shí)間: 2025-3-22 01:18 作者: 易受騙 時(shí)間: 2025-3-22 04:40 作者: Offset 時(shí)間: 2025-3-22 09:42 作者: 含糊 時(shí)間: 2025-3-22 16:23
Boron Isotopic composition?of Pegmatitic Tourmaline from Yumthang Valley, North Sikkim, Indiaotal REE and Type 2: having [(La/Yb). from (1.88 to 6.63)]. The δ.B values of the studied pegmatitic tourmalines are similar to that of the continental crust and S-type granites and ranges from???13.83?±?0.37 ‰ to???12.78?±?0.84 ‰ suggesting crustal origin. The low δ.B values from the studied tourma作者: 含糊 時(shí)間: 2025-3-22 18:46
Geochemistry and U–Pb CHIME Ages of Tonalite–Trondhjemitic–Granodioritic (TTG) Gneiss from the Centrent shows enriched nature, while HFS elements show depletion. Based on HREE concentration, the compiled TTG gneisses data from Central Bundelkhand terrane are further classified into three groups as low HREE (TTG-I), high HREE (TTG-II), and medium HREE (TTG-III). The protoliths of TTG gneisses are i作者: BOOST 時(shí)間: 2025-3-23 00:22
The Geochemical Affinity of Paleogene Glauconites in Paleo-Tethyan Deposits of Indias show a wide variation in major oxide contents, viz. K.O (3.09–8.65?wt%), Fe.O. (15.33–29.49?wt%), Al.O. (5.12–16.77?wt%), MgO (2.06–9.00?wt%), and SiO. (39.16–57.02?wt%). The chemical composition of the glauconite, therefore, encompasses the entire range of K-poor to K-rich glauconite, supporting 作者: fatty-acids 時(shí)間: 2025-3-23 02:52
Paleoenvironmental Dynamics in a Mesoproterozoic Epicontinental Sea, Faded Shale, Son Valley, Indiain refractory elements, although both are now vertically juxtaposed in the same paleogeography. The majority of samples display MREE enrichment presumably because of organic matter (OM) abundance. The ST facies, apparently bears geochemical signature of the shallow shelf. Various paleoredox-sensitiv作者: outer-ear 時(shí)間: 2025-3-23 08:15
Detrital Zircon Geochemistry in the Morita Formation, Northern Sonora, Mexico: Implications for Origcons show depleted LREE and very strongly enriched HREE patterns with positive Ce and negative Eu anomalies. The presence of significant negative Eu anomalies in these zircons suggest also that they were largely contributed by granitoids sources. Some zircons have relatively flat LREE and very stron作者: charisma 時(shí)間: 2025-3-23 10:21
Geochemistry and Petrological Studies of the Mesoproterozoic Glauconitic Sandstone, Semri Group, Vinration of K for the formation of glauconite. Al.O./TiO. ratio of glauconite rocks suggests its derivation from felsic source rocks. The ratio Al.O./SiO.?>?5 of glauconitic sandstone shows low to moderate maturity revealing the tectonic process during sedimentation. The tectonic discrimination diagra作者: 辭職 時(shí)間: 2025-3-23 17:39 作者: micturition 時(shí)間: 2025-3-23 18:44 作者: JUST 時(shí)間: 2025-3-23 22:30
https://doi.org/10.1007/978-3-662-41391-3(<8) with high Al.O., K.O, Rb and Th confirm the crustal contamination coupled with the fractional crystallization process in the generation of the felsic volcanic rocks. The mafic volcanic rocks of this belt correspond to back arc regime with a MORB composition, whereas active continental margin is作者: 包庇 時(shí)間: 2025-3-24 05:30 作者: 細(xì)胞 時(shí)間: 2025-3-24 09:22 作者: 浪費(fèi)時(shí)間 時(shí)間: 2025-3-24 11:38 作者: tooth-decay 時(shí)間: 2025-3-24 15:11 作者: GEM 時(shí)間: 2025-3-24 20:48 作者: 創(chuàng)作 時(shí)間: 2025-3-25 00:31 作者: incontinence 時(shí)間: 2025-3-25 07:00 作者: obnoxious 時(shí)間: 2025-3-25 11:02
Die Idee der Relativit?tstheoriein refractory elements, although both are now vertically juxtaposed in the same paleogeography. The majority of samples display MREE enrichment presumably because of organic matter (OM) abundance. The ST facies, apparently bears geochemical signature of the shallow shelf. Various paleoredox-sensitiv作者: 某人 時(shí)間: 2025-3-25 12:12
https://doi.org/10.1007/978-3-7091-4020-8cons show depleted LREE and very strongly enriched HREE patterns with positive Ce and negative Eu anomalies. The presence of significant negative Eu anomalies in these zircons suggest also that they were largely contributed by granitoids sources. Some zircons have relatively flat LREE and very stron作者: 反對 時(shí)間: 2025-3-25 18:47
Die scheinbare Absurdit?t dieser Folgerungenration of K for the formation of glauconite. Al.O./TiO. ratio of glauconite rocks suggests its derivation from felsic source rocks. The ratio Al.O./SiO.?>?5 of glauconitic sandstone shows low to moderate maturity revealing the tectonic process during sedimentation. The tectonic discrimination diagra作者: Synchronism 時(shí)間: 2025-3-25 22:23
https://doi.org/10.1007/978-3-642-61848-2 (d) G4: acid rocks, and (e) G5: disequilibrium rocks. Each group has been evaluated in terms of rock classification, spatial distribution, approximation of intensive properties (pressure and temperature), magmatic process inference, and tectonic setting. Petrogenesis of extensional-related G1 and G作者: 糾纏,纏繞 時(shí)間: 2025-3-26 03:35 作者: 敘述 時(shí)間: 2025-3-26 07:34 作者: 哄騙 時(shí)間: 2025-3-26 11:49
Book 2022r, trace and rare earth elements in rocks to identify the magmatic processes involved in present-day magma generation and their relation to global tectonic regimes as well as geothermal studies. Therefore, the book provides a comprehensive view of the generation of magma types (mafic to felsic in co作者: Arable 時(shí)間: 2025-3-26 12:46 作者: 夜晚 時(shí)間: 2025-3-26 19:30 作者: 基因組 時(shí)間: 2025-3-26 23:46 作者: 一大塊 時(shí)間: 2025-3-27 02:21 作者: craven 時(shí)間: 2025-3-27 08:53 作者: ANTE 時(shí)間: 2025-3-27 10:41 作者: 運(yùn)動(dòng)吧 時(shí)間: 2025-3-27 16:40 作者: infringe 時(shí)間: 2025-3-27 18:43
https://doi.org/10.1007/978-3-662-41391-3he mafic rocks are composed of amphibole and plagioclase with minor amount of quartz and pyroxene, whereas the felsic rocks consist of K-feldspars, quartz and plagioclase. These are geochemically distinguished as basalts and dacites in which the silica content of the mafic volcanic rocks ranges from作者: Nebulous 時(shí)間: 2025-3-27 23:23 作者: 畸形 時(shí)間: 2025-3-28 05:20
Walther Wegener F. T. I.,Rolf Gusesent new petrography and whole-rock geochemistry for felsic volcanic rocks to understand their origin, evolution, petrogenesis and their tectonic relation with the MC. Based on geochemical composition, these rocks are divided into two main groups: (i) rhyolite and (ii) trachydacite, respectively. Th作者: 勉強(qiáng) 時(shí)間: 2025-3-28 09:58 作者: 監(jiān)禁 時(shí)間: 2025-3-28 10:26 作者: 陪審團(tuán)每個(gè)人 時(shí)間: 2025-3-28 18:27
R. Stücker,W. Konermann,G. U. Exnerhanashini estuaries, along the central western coast of India, were investigated to understand the source, processes, and depositional environments. The distribution and abundance of parameters studied reveal that they were controlled largely by the catchment area geology, geomorphology, and estuari作者: BILE 時(shí)間: 2025-3-28 18:51
,Periartikul?re Verkn?cherungen,057?m, ~3542?m, ~3726?m, and ~3738?m water depth, respectively). The grain size, mineralogy, geochemistry, and radiocarbon ages of the sediment cores were analyzed. N57 and N59 cores were characterized by detrital components enriched in SiO., Al.O., and Fe.O. contents. On the other hand, the N60, N6作者: 積極詞匯 時(shí)間: 2025-3-29 00:49 作者: 窩轉(zhuǎn)脊椎動(dòng)物 時(shí)間: 2025-3-29 06:12 作者: 冒失 時(shí)間: 2025-3-29 09:21
Portal und Multi-Provider-Managementestigation of the Paleogene glauconites in India. The biostratigraphic data reflects the overlapping temporal distribution of the Paleogene glauconitic rocks of Kutch, Cambay, Jaisalmer, Barmer, and Assam-Arakan basins, viz. late Paleocene-early Eocene, middle Eocene, and late Oligocene. In sharp co作者: connoisseur 時(shí)間: 2025-3-29 12:58 作者: 毗鄰 時(shí)間: 2025-3-29 16:49
https://doi.org/10.1007/978-3-7091-4020-8n the localities of Sierra Anibacachi and Rancho Bufalo in northeastern Sonora to infer origin and source rocks type of their sediments. Zircon grains show large variations in P, Ti, Y, U, Th and Hf concentrations, while ΣREE concentrations in zircons vary significant from sample to sample. Zircon c作者: 真繁榮 時(shí)間: 2025-3-29 21:54 作者: Loathe 時(shí)間: 2025-3-30 00:03 作者: Innocence 時(shí)間: 2025-3-30 04:29 作者: Alcove 時(shí)間: 2025-3-30 11:44 作者: MILK 時(shí)間: 2025-3-30 13:14 作者: 高腳酒杯 時(shí)間: 2025-3-30 16:37 作者: 彎彎曲曲 時(shí)間: 2025-3-30 20:48 作者: 使成整體 時(shí)間: 2025-3-31 01:47 作者: epicondylitis 時(shí)間: 2025-3-31 06:37
Importance of the Geochemistry of Nearshore Sediments in the Realm of Heavy Metal Pollution Assessmendwater with the seawater, diagenetic remobilization/re-suspension of sediments, landward transport of marine sediments and atmospheric deposition. Hence, estuarine sediments are much complicated in their chemistry because of the dynamics and chemical processes involved in their formation combined w作者: 極大痛苦 時(shí)間: 2025-3-31 10:52
