標(biāo)題: Titlebook: Geodynamic Evolution of the Indian Shield: Geophysical Aspects; Om Prakash Pandey Book 2020 Springer Nature Switzerland AG 2020 Seismogene [打印本頁(yè)] 作者: BROOD 時(shí)間: 2025-3-21 16:19
書目名稱Geodynamic Evolution of the Indian Shield: Geophysical Aspects影響因子(影響力)
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書目名稱Geodynamic Evolution of the Indian Shield: Geophysical Aspects網(wǎng)絡(luò)公開(kāi)度學(xué)科排名
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書目名稱Geodynamic Evolution of the Indian Shield: Geophysical Aspects讀者反饋
書目名稱Geodynamic Evolution of the Indian Shield: Geophysical Aspects讀者反饋學(xué)科排名
作者: 講個(gè)故事逗他 時(shí)間: 2025-3-21 20:21 作者: 徹底明白 時(shí)間: 2025-3-22 02:23
2194-9204 s latest findings on the geodynamic development of the Indian shield and nearby continental margins, including Arabian Sea..978-3-030-40599-1978-3-030-40597-7Series ISSN 2194-9204 Series E-ISSN 2194-9212 作者: Intrepid 時(shí)間: 2025-3-22 07:30
Rekurrensimpfbehandlung der Paralyse,nd magmatism, followed by crustal extension, rifting and subsidence due to episodic thermal interaction of the crust with the hot underlying mantle.This basin apparently evolved as a foreland basin on a rifted Indian crust, caused by continued crustal extension. Geophysicall, this basin is well studied.作者: CANE 時(shí)間: 2025-3-22 10:50 作者: Evacuate 時(shí)間: 2025-3-22 14:45
https://doi.org/10.1007/978-3-662-00286-5physical (seismic, gravity, magnetic, heat flow, MT etc) and aftershock studies were undertaken over these seismic zones, which indicate that most of these regions are in state of continuous uplift and erosion, which have brought mafic crust (amphiolitic-granulitic) quite close to surface, in which stresses are getting accumulated.作者: Evacuate 時(shí)間: 2025-3-22 18:09
Schlussbetrachtung und Ausblick 100 km. These findings re-affirm that the Indian crust, as well as mantle, is quite warm due to rise of isotherms at shallow level. Thinning of the Indian lithosphere may be due to the combination of both, Deccan volcanic event and continued lithospheric remobilization since Midproterozoic period.作者: 主講人 時(shí)間: 2025-3-23 01:12
Vindhyan Basin: Anomalous Crust-Mantle Structure,nd magmatism, followed by crustal extension, rifting and subsidence due to episodic thermal interaction of the crust with the hot underlying mantle.This basin apparently evolved as a foreland basin on a rifted Indian crust, caused by continued crustal extension. Geophysicall, this basin is well studied.作者: Demulcent 時(shí)間: 2025-3-23 01:35
Seismic, Elastic and Petrophysical Properties of Crustal Rocks: Deccan Volcanic Province,xperiencing high level of intraplate seismic activity. Deep scientific drillings in two such prominent seismic zones, provided unique opportunity to study such properties. Results obtained on Deccan volcanic and basement cores from 617 m deep Killari borehole, have given some very interesting clues to geological evolution of this terrain.作者: 純樸 時(shí)間: 2025-3-23 09:37 作者: regale 時(shí)間: 2025-3-23 12:03 作者: 確定無(wú)疑 時(shí)間: 2025-3-23 14:51 作者: 叫喊 時(shí)間: 2025-3-23 18:42
Geodynamic and Geologic Evolution of Indian Continent: A Brief History,arried out in Deccan volcanic terrain, which is considered one of the largest flood basaltic provinces on the surface of the Earth. Historically, it has been associated with a moderate intraplate seismic activity, usually not found in stable continental regions. Such unusual characters are very well reflected in all the geophysical fields.作者: Collected 時(shí)間: 2025-3-23 22:49
Book 2020al studies, like seismic, seismological, gravity, magnetic, magnetotelluric and heat flow, carried out over the past five decades. Further, it discusses elastic and petrophysical properties of the Earth’s crust relevant to geological investigations. The book also shares latest findings on the geodyn作者: Servile 時(shí)間: 2025-3-24 04:53
https://doi.org/10.1007/978-3-662-42515-2in the world. It is associated with distinct geologic, geotectonic and magmatic signatures. Indian shield underwent large scale deformation and degeneration at crust and lithospheric mantle level, due to sustained thermo-geodynamic perturbations, specially during the Cretaceous period, when the Eart作者: 全面 時(shí)間: 2025-3-24 06:46 作者: FOR 時(shí)間: 2025-3-24 14:38
Malaria biliosa haemoglobinurica,d active mobile belts. More than four decades ago, it was postulated through some studies that the Indian shield does not possess characteristics of a typical stable shield terrain. Out of these two cratons, Singhbhum craton, is perhaps the finest example of that, which forms one of the most deforme作者: Ccu106 時(shí)間: 2025-3-24 17:45 作者: 樹膠 時(shí)間: 2025-3-24 19:46
Rekurrensimpfbehandlung der Paralyse,ontinental shields and platform areas world-wide. Indian subcontinent contains four of them. All these basins came into existence due to sustained rifting and subsidence of the central part of the Indian peninsular shield. Out of these, the Vindhyan basin, located in central India and containing thi作者: 古文字學(xué) 時(shí)間: 2025-3-25 02:38 作者: minaret 時(shí)間: 2025-3-25 07:05
Die Malariatherapie der kongenitalen Lues,and seismic wave attenuation, is extremely important to study various geophysical and geodynamical problems. Since major part of the Earth’s continental crust, remains inaccessible to direct observations, the laboratory measurement of such properties becomes essential, which are used to model the cr作者: Optometrist 時(shí)間: 2025-3-25 09:57
https://doi.org/10.1007/978-3-662-00286-5ian Stable Continental Region (SCR) experiences moderate-to-large intraplate seismic activity since historical times. Most of the past earthquakes e.g.,1819 Kachchh, 1927 Son-valley, 1967 Koyna, 1970 Broach, 1993 Killari, 1997 Jabalpur and 2001 Bhuj among many others, have occurred over the regions 作者: Obliterate 時(shí)間: 2025-3-25 13:52 作者: Alopecia-Areata 時(shí)間: 2025-3-25 18:31
https://doi.org/10.1007/978-3-663-02186-5f its time-bound evolution, as well as interpretation of acquired geological and geophysical data. Structural fabric and composition of the crust have undergone considerable changes since Archean era. Almost 5 to 20 km thick upper portion of the crust is eroded away from several Archean-Proterozoic 作者: 榨取 時(shí)間: 2025-3-25 22:41
978-3-030-40599-1Springer Nature Switzerland AG 2020作者: 貿(mào)易 時(shí)間: 2025-3-26 03:40 作者: gain631 時(shí)間: 2025-3-26 07:11 作者: blight 時(shí)間: 2025-3-26 10:52 作者: 供過(guò)于求 時(shí)間: 2025-3-26 15:30 作者: Decongestant 時(shí)間: 2025-3-26 19:54
Malaria biliosa haemoglobinurica,terized by anomalous geophysical signatures, like high gravity bias and high heat flow. It also has an unusually thin (65–100 km) and warm lithosphere, as a result of shearing and degeneration by the buoyant hot mantle.作者: 清洗 時(shí)間: 2025-3-26 21:48 作者: Affection 時(shí)間: 2025-3-27 03:01
Rekurrensimpfbehandlung der Paralyse,t flow and number of hot springs, besides high level of intraplate seismicity, including Reservoir Triggerd Seismicity (RTS) as well. Crust-mantle structure below this region is severely affected by Deccan volcanism and associated geodynamic phenomena.作者: 卡死偷電 時(shí)間: 2025-3-27 07:42 作者: 吹氣 時(shí)間: 2025-3-27 12:16
Dharwar Craton, and accretion, rifting, continent-continent collision, suturing and basaltic magma extrusion. Inner parts of this craton may have been rifting as late as in Gondwana period, challenging the wide held belief of cratonic instability.作者: 新奇 時(shí)間: 2025-3-27 17:40
Singhbhum and Bastar Cratons,terized by anomalous geophysical signatures, like high gravity bias and high heat flow. It also has an unusually thin (65–100 km) and warm lithosphere, as a result of shearing and degeneration by the buoyant hot mantle.作者: 鐵砧 時(shí)間: 2025-3-27 19:06
Aravalli and Bundelkhand Cratons,ing the Paleoproterozoic period, Bundelkhand cratonic micro-plate started subducting below the Mesoarchean Mewar terrain of the Aravalli craton; the collision between these two blocks was possibly responsible for the development of the Aravalli mountain ranges.作者: Psychogenic 時(shí)間: 2025-3-27 22:02
Western Continental Margin and Adjacent Oceanic Regions,t flow and number of hot springs, besides high level of intraplate seismicity, including Reservoir Triggerd Seismicity (RTS) as well. Crust-mantle structure below this region is severely affected by Deccan volcanism and associated geodynamic phenomena.作者: Preamble 時(shí)間: 2025-3-28 03:53 作者: magenta 時(shí)間: 2025-3-28 10:18 作者: 縫紉 時(shí)間: 2025-3-28 13:32 作者: 努力趕上 時(shí)間: 2025-3-28 14:56 作者: GOAD 時(shí)間: 2025-3-28 19:10
Singhbhum and Bastar Cratons,d active mobile belts. More than four decades ago, it was postulated through some studies that the Indian shield does not possess characteristics of a typical stable shield terrain. Out of these two cratons, Singhbhum craton, is perhaps the finest example of that, which forms one of the most deforme作者: legacy 時(shí)間: 2025-3-29 00:58
Aravalli and Bundelkhand Cratons,Indian peninsular shield, having undergone paleo-subduction, continent-continent collision, multiple folding and active deformation. Geophysically, it is one of the most unusual, somewhat similar to the Singhbhum craton. Considerable amount of geophysical work has thus been carried out over this ter作者: 碳水化合物 時(shí)間: 2025-3-29 03:18 作者: 虛弱的神經(jīng) 時(shí)間: 2025-3-29 07:34 作者: agonist 時(shí)間: 2025-3-29 15:29
Seismic, Elastic and Petrophysical Properties of Crustal Rocks: Deccan Volcanic Province,and seismic wave attenuation, is extremely important to study various geophysical and geodynamical problems. Since major part of the Earth’s continental crust, remains inaccessible to direct observations, the laboratory measurement of such properties becomes essential, which are used to model the cr作者: 繁忙 時(shí)間: 2025-3-29 16:38 作者: Contort 時(shí)間: 2025-3-29 22:04
Heat Flow and Lithospheric Thermal Structure, India, has been a subject of considerable interest. So far, heat flow is evaluated for over 170 locations over this terrain, which regionally varies from a low of 23.0 mW/m. to as high as 107.0 mW/m.. Their distribution conforms well with the nature of underlying crust and mantle inhomogeneities. A作者: manifestation 時(shí)間: 2025-3-30 01:34 作者: ineluctable 時(shí)間: 2025-3-30 04:32
