標題: Titlebook: Geological Evolution of the Precambrian Indian Shield; M.E.A. Mondal Book 2019 Springer International Publishing AG, part of Springer Natu [打印本頁] 作者: TOUT 時間: 2025-3-21 18:49
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書目名稱Geological Evolution of the Precambrian Indian Shield影響因子(影響力)學科排名
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書目名稱Geological Evolution of the Precambrian Indian Shield讀者反饋
書目名稱Geological Evolution of the Precambrian Indian Shield讀者反饋學科排名
作者: integrated 時間: 2025-3-21 22:58 作者: 推測 時間: 2025-3-22 01:00
,Zircon U–Pb (SHRIMP) Ages of the Jahazpur Granite and Mangalwar Gneiss from the Deoli-Jahazpur Sectgranite. Concomitant metamorphism and granitic magmatism imply that overlying Hindoli-Jahazpur Group is younger than c. 2520?Ma. Thus, the Neoarchean Jahazpur granite and Mangalwar gneiss are constituents of the Banded Gneissic Complex which forms the basement of the Hindoli-Jahazpur supracrustal sequence.作者: organic-matrix 時間: 2025-3-22 04:33 作者: 禁止,切斷 時間: 2025-3-22 09:45
,Geochemistry of Mafic–Felsic Rocks of Phulad Ophiolite, in and Around Pindwara-Mount Abu Region, Sosent and well preserved in the area. With the help of systematic field mapping, a complete sequence has been reconstructed. New geochemical data in conjunction with published data affirms fore arc tectonic setting of this sequence.作者: 排斥 時間: 2025-3-22 14:49 作者: 排斥 時間: 2025-3-22 19:23 作者: 香料 時間: 2025-3-22 21:56
Book 2019leobiological data from the rocks in the Precambrian shield area, and presents a collection of contributions on these diverse topics that help to reconstruct the Precambrian evolution of the Indian Shield..作者: 嬰兒 時間: 2025-3-23 05:23
https://doi.org/10.1007/978-3-030-55400-2ian crustal blocks which together constituted the Proto-India include Dharwar, Bastar, Singhbhum, Rajmahal, Bundelkhand, and Aravalli. The Protocontinents are separated from each other by Joins marked by Lineament like the Narmada-Son, or by the Gondwana rift basins like the Godavari, Mahanadi and t作者: 盡責 時間: 2025-3-23 09:15 作者: ZEST 時間: 2025-3-23 12:49 作者: 倒轉 時間: 2025-3-23 15:08 作者: 周年紀念日 時間: 2025-3-23 20:55
The Role of Complementary Protectionrred to be braided, channels possibly become more sinuous towards the top of the succession, as inferred from the appearance of bank-attached bars along with the omnipresent longitudidal bars. Flow durability within channel also increases with time, as the lower two belts appear to be ephemeral with作者: 切掉 時間: 2025-3-24 00:27 作者: 歌唱隊 時間: 2025-3-24 06:01
https://doi.org/10.1007/978-3-030-50597-4 TTG exhibit: (i) highly fractionated rare earth element (REE) patterns; and (ii) negative anomalies of Nb and Ti. These geochemical characteristics of the TTG suggest that they were not produced from partial melting of mid-oceanic ridge basalts/normal oceanic crust. Instead we propose that the TTG 作者: 新娘 時間: 2025-3-24 08:02
International Law in the Western Hemisphereical, fluidal and alterational characteristics closely resembling IOCG settings. Their timing and other similarities possibly indicate a major crustal scale event of brecciation associated with ascent of magmatically derived hydrothermal fluids and extensive epithermal alteration of host rocks. Thes作者: 消散 時間: 2025-3-24 14:11 作者: 健談的人 時間: 2025-3-24 16:17 作者: decode 時間: 2025-3-24 21:54 作者: 蒙太奇 時間: 2025-3-25 00:44 作者: laceration 時間: 2025-3-25 04:55 作者: 痛打 時間: 2025-3-25 11:13
https://doi.org/10.1007/978-1-137-09829-0 rare minute erosional features at its base. Non-luminiscent character of the former under CL is reminiscent of oxidizing basin-floor environment, while the bright orange luminescence of the latter testifies pervasive burial recrystallization. The dark micritic facies is interpreted as indigenous an作者: slipped-disk 時間: 2025-3-25 13:20
https://doi.org/10.1007/978-1-349-24295-5terns along with prominent negative Eu anomaly [pelitic gneisses: La./Yb.?=?19.7 ? 81.7, Eu/Eu*?=?0.17 ? 0.68; pelitic schist: La./Yb.?=?27.4 ? 43.7, Eu/Eu*?=?0.15 ? 0.32]. Post-Archean Australian Shale (PAAS) normalized multi-element diagram for the pelitic gneisses exhibits enrichment of Nb, Th, C作者: Sad570 時間: 2025-3-25 16:12 作者: Chronological 時間: 2025-3-25 19:59 作者: 苦惱 時間: 2025-3-26 00:28
Indian Shield: Pristine Shape, Size and Tectonic Framework,ian crustal blocks which together constituted the Proto-India include Dharwar, Bastar, Singhbhum, Rajmahal, Bundelkhand, and Aravalli. The Protocontinents are separated from each other by Joins marked by Lineament like the Narmada-Son, or by the Gondwana rift basins like the Godavari, Mahanadi and t作者: Ingredient 時間: 2025-3-26 07:26 作者: plasma 時間: 2025-3-26 08:27 作者: 倔強不能 時間: 2025-3-26 13:52 作者: ATRIA 時間: 2025-3-26 19:26 作者: 確定的事 時間: 2025-3-26 21:20 作者: AND 時間: 2025-3-27 02:41 作者: Ischemia 時間: 2025-3-27 06:04 作者: Antigen 時間: 2025-3-27 13:01 作者: 比喻好 時間: 2025-3-27 17:30 作者: 貞潔 時間: 2025-3-27 20:09
Controls on Cyclic Sedimentation Within the Neoproterozoic Sirbu Shale, Vindhyan Basin, Central Indas a Highstand Systems Tract (HST). Intrinsic studies unravel that the interval incorporates two different orders of high frequency cyclicities, in terms of parasequence and parasequence sets. The parasequences are genetically related shoaling-upward successions bounded by marine flooding surfaces a作者: 綁架 時間: 2025-3-27 22:23
Trace, Rare-Earth Elements and C, O Isotope Systematics of Carbonate Rocks of Proterozoic Bhima Gromical modeling suggests (1) little influence (<1%) of clastic material on REY systematics, (2) significant contribution (~>10%) of river/estuarine run-off to the ambient sea water and possibly minor input from oceanic hydrothermal sources. High positive values of δ.C (3.8‰) in the basal Shahabad car作者: 輕率看法 時間: 2025-3-28 04:25 作者: Expand 時間: 2025-3-28 08:10 作者: 壁畫 時間: 2025-3-28 11:24 作者: Anticoagulants 時間: 2025-3-28 15:30 作者: chlorosis 時間: 2025-3-28 20:09 作者: 預防注射 時間: 2025-3-29 00:01
Geological Evolution of the Precambrian Indian Shield作者: MELON 時間: 2025-3-29 04:19 作者: 多余 時間: 2025-3-29 09:57
Evolution of the Indian Shield: A New Approach,ravalli craton (AC), all comprising greenstone-gneiss in different abundance ratios. As in other Archean terrains, this ocean-continental rock association dichotomy is explained by extrusion of mafic lava and its transformation into greenstone along with its melting at depth to generate tonalitic ma作者: 發(fā)出眩目光芒 時間: 2025-3-29 13:21
,Zircon U–Pb (SHRIMP) Ages of the Jahazpur Granite and Mangalwar Gneiss from the Deoli-Jahazpur Secte Aravalli Craton, northwestern India. These data are useful to understand the stratigraphic correlation between the basement gneiss and the low-grade supracrustal rocks of the Hindoli-Jahazpur Group. U–Pb (SHRIMP-IIe) data from zircon suggest emplacement age of 2538?±?5?Ma for the Jahazpur granite,作者: peritonitis 時間: 2025-3-29 18:03 作者: MUMP 時間: 2025-3-29 20:13
,Mineral Chemistry, Sr–Nd Isotope Geochemistry and Petrogenesis of the Granites of Bathani Volcano-Sgpur Granite Gneiss Complex of Central Indian Tectonic Zone has been presented in this paper to understand its petrogenesis and implications for crustal growth in the eastern Indian shield. Petrographically, they are coarse-grained granites with biotite, plagioclase feldspar and K-feldspar as major 作者: 改革運動 時間: 2025-3-30 01:27
Stratigraphic Evolution and Architecture of the Terrestrial Succession at the Base of the Neoproteruilding pattern within the ambit of the Precambrian fluvial sedimentation system. Detailed facies, architectural element, paleocurrent as well as stratigraphic architectural analysis invariably revealed a frequently avulsive braided pattern, with flashy discharges, for the paleoriver system; which i作者: 產(chǎn)生 時間: 2025-3-30 06:15
Deformation and Tectonic History of Punagarh Basin in the Trans-Aravalli Terrane of North-Western Ieformed and metamorphosed basement rocks of Sojat Formation. The basement rocks were deformed into upright inclined folds with parallel to chevron geometry. The axial plane cleavages were developed showing variation in trend from NE-SW to ENE-WSW and this variation was due to late generation open fo作者: 音樂戲劇 時間: 2025-3-30 08:56 作者: dry-eye 時間: 2025-3-30 13:24 作者: NOVA 時間: 2025-3-30 17:01
Deformation of Pyrite at Varying Metamorphic Grades in Sediment-Hosted Base Metal Sulphide Depositsen. Very often it shares the deformational and metamorphic history of its host rocks. Textural characteristics of pyrite, and its behavior in natural ores and in experimental conditions under varying temperature and pressure, have therefore been studied by different workers from time to time. An ove作者: 聯(lián)合 時間: 2025-3-30 22:48
Provenance and Tectonic Setting of the Proterozoic Clastic Rocks of the Kerur Formation, Badami Grognatures. The lithology of the Kerur Formation includes basal arenite (BA), lower conglomerate (LC), quartz arenite (QA) and upper conglomerate (UC). The CIA and PIA values and A–CN–K diagram indicate a moderate to intense chemical weathering for the clastic rocks of the Kerur Formation. The bivaria作者: mechanical 時間: 2025-3-31 02:34 作者: Baffle 時間: 2025-3-31 05:00 作者: 對手 時間: 2025-3-31 10:19 作者: 規(guī)范就好 時間: 2025-3-31 15:42 作者: 拋棄的貨物 時間: 2025-3-31 19:50
