標題: Titlebook: Geology of the Nepal Himalaya; Regional Perspective Megh Raj Dhital Book 2015 Springer International Publishing Switzerland 2015 Ganga Basi [打印本頁] 作者: ED431 時間: 2025-3-21 16:40
書目名稱Geology of the Nepal Himalaya影響因子(影響力)
書目名稱Geology of the Nepal Himalaya影響因子(影響力)學科排名
書目名稱Geology of the Nepal Himalaya網(wǎng)絡(luò)公開度
書目名稱Geology of the Nepal Himalaya網(wǎng)絡(luò)公開度學科排名
書目名稱Geology of the Nepal Himalaya被引頻次
書目名稱Geology of the Nepal Himalaya被引頻次學科排名
書目名稱Geology of the Nepal Himalaya年度引用
書目名稱Geology of the Nepal Himalaya年度引用學科排名
書目名稱Geology of the Nepal Himalaya讀者反饋
書目名稱Geology of the Nepal Himalaya讀者反饋學科排名
作者: Admonish 時間: 2025-3-22 00:09 作者: JAMB 時間: 2025-3-22 02:40 作者: Fortuitous 時間: 2025-3-22 05:13
Geological Setting of Himalaya, flysch complexes, and island arcs in Tibetan Plateau; Qilian Shan terrane, Kunlun–Qaidam terrane, Songpan–Ganzi terrane, Qiantang terrane, and Lhasa terrane; Indus–Tsangpo suture zone; Himalayan orogen and its main features; Ganga foreland basin—south border of Himalaya; basement structure of Gang作者: 察覺 時間: 2025-3-22 09:27 作者: bleach 時間: 2025-3-22 13:00
Northwest Himalaya Auden on Krol Belt; Shali window: West’s version; Further investigations in Simla–Krol belt; Pre-Tertiary outliers in Sub-Himalaya; Lithostratigraphic correlation and other issues: Simla Slates and allied rocks, Blaini boulderbeds, carbonate sequences, depositional environment of Simla Slates and K作者: bleach 時間: 2025-3-22 20:15
Southeast Himalaya and Adjacent Indian Peninsulaian Peninsula; Lower Gondwanas: Talchir Formation and Damudas; Middle Gondwanas: Panchet, Mahadeva, and Maleri formations; Upper Gondwanas and Rajmahal traps; Lesser Himalayan sequence: Daling and Shumar groups, Baxa Formation, Diuri Formation, Setikhola Formation, Damudas; Higher Himalayan crystall作者: intricacy 時間: 2025-3-22 22:20 作者: Missile 時間: 2025-3-23 03:43 作者: 表兩個 時間: 2025-3-23 05:53
Lesser Himalaya of Karnali–Bheri Regiononic window within Great Midland Antiform; window containing Chail nappes of Fuchs; antiformal core between Sinja and Lake Rara; Surkhet–Dailekh tract containing Early Miocene rocks and Proterozoic carbonates of Lakharpata Group; Ranimatta Formation with basic rocks; fossiliferous beds of Barikot wi作者: 生命層 時間: 2025-3-23 12:32 作者: 藐視 時間: 2025-3-23 15:11
Lesser Himalaya of Arun–Tamar Region, quartzites, phyllites, and calc-schists; Lesser Himalayan sequence of Sabha Khola area comprising Tumlingtar Group, Chainpur Group, and Phakuwa Group; Taplejung window exposing low-grade metamorphic rocks of Taplejung Group and mylonitic gneisses; Proterozoic granites and granitic gneisses in core作者: 空氣傳播 時間: 2025-3-23 19:22
Introduction to Higher Himalaya Cross-section of Kruparz through Kathmandu and Nyalam; Upper Crystalline nappe; recognition of Main Central Thrust; central gneiss versus gneissose granite; Composition of Higher Himalayan crystallines; Gosainkund tectonic bridge; deformation in Main Central Thrust zone; folded Higher Himalayan thr作者: 松軟 時間: 2025-3-24 00:56 作者: 代替 時間: 2025-3-24 03:15 作者: itinerary 時間: 2025-3-24 08:11 作者: 旁觀者 時間: 2025-3-24 11:55
https://doi.org/10.1057/9781137393630isions of Nepal; upper, middle, and lower Terai; Siwaliks and dun valleys; single and multiple Siwalik ranges; Mahabharat Range and its three segments; Midlands; Fore Himalaya; Great Himalaya; inner Himalayan valleys; Tibetan marginal ranges.作者: Invigorate 時間: 2025-3-24 18:00 作者: 我沒有強迫 時間: 2025-3-24 20:49
The Networked Educator and Open Learning,ian Peninsula; Lower Gondwanas: Talchir Formation and Damudas; Middle Gondwanas: Panchet, Mahadeva, and Maleri formations; Upper Gondwanas and Rajmahal traps; Lesser Himalayan sequence: Daling and Shumar groups, Baxa Formation, Diuri Formation, Setikhola Formation, Damudas; Higher Himalayan crystall作者: Bronchial-Tubes 時間: 2025-3-25 01:13
On the Development of Digital Memories Tethys and Oligocene–Miocene continental deposits; more than 200?km wide Miocene foreland basin; pioneer investigations; great controversy; distribution of Lesser Himalayan sequence: tectonic windows, inner zone, intermediate zone, and outer zone; Proterozoic slices in Sub-Himalaya; classifying Les作者: Platelet 時間: 2025-3-25 06:46
https://doi.org/10.1007/978-3-031-10698-9e with overturned strata and northerly Chamoli–Tejam zone; investigations between Darchula and Budar: Malikarjun Thrust and Early Miocene strata, Baitadi Carbonates and Patan Formation, early Tertiary beds of Patan–Pancheshwar, and Budar–Gaira Transect.作者: 陶器 時間: 2025-3-25 09:30 作者: Camouflage 時間: 2025-3-25 13:54 作者: Foreknowledge 時間: 2025-3-25 19:46 作者: Instantaneous 時間: 2025-3-25 21:11 作者: 鍍金 時間: 2025-3-26 00:11 作者: Gobble 時間: 2025-3-26 07:36
Wolfgang Appel,Birgit Michel-DittgenThe Lesser Himalayan rocks of the Bagmati–Gosainkund region compose a relatively wide portion of the Great Midland Antiform in the inner zone between Nuwakot and Dhunche, and they also form an open fold representing the Great Mahabharat Synform in the intermediate zone around Mugling and Narayanghat.作者: 缺乏 時間: 2025-3-26 11:10 作者: 配置 時間: 2025-3-26 15:21 作者: 方便 時間: 2025-3-26 19:51 作者: 彎曲道理 時間: 2025-3-27 00:55 作者: 花費 時間: 2025-3-27 04:26 作者: Decimate 時間: 2025-3-27 07:26 作者: 機械 時間: 2025-3-27 12:37
https://doi.org/10.1057/9781137393630isions of Nepal; upper, middle, and lower Terai; Siwaliks and dun valleys; single and multiple Siwalik ranges; Mahabharat Range and its three segments; Midlands; Fore Himalaya; Great Himalaya; inner Himalayan valleys; Tibetan marginal ranges.作者: HUMP 時間: 2025-3-27 16:26
Contexts, Practices and Pedagogies, Auden on Krol Belt; Shali window: West’s version; Further investigations in Simla–Krol belt; Pre-Tertiary outliers in Sub-Himalaya; Lithostratigraphic correlation and other issues: Simla Slates and allied rocks, Blaini boulderbeds, carbonate sequences, depositional environment of Simla Slates and Krol Formation, Subathu–Dagshai passage-beds.作者: interference 時間: 2025-3-27 21:30 作者: Grating 時間: 2025-3-27 23:39 作者: 歡笑 時間: 2025-3-28 03:04 作者: genuine 時間: 2025-3-28 06:40 作者: 我的巨大 時間: 2025-3-28 13:33 作者: Prologue 時間: 2025-3-28 18:36 作者: thalamus 時間: 2025-3-28 22:10 作者: 不來 時間: 2025-3-28 23:18 作者: 不能約 時間: 2025-3-29 03:51 作者: 談判 時間: 2025-3-29 09:04
On the Development of Digital Memoriesser Himalayan rocks; Proterozoic augen gneisses and granites; carbonate sequences; correlation of unfossiliferous rocks; Gondwanas; inverted metamorphism; structure of inner, intermediate, and outer zones; Main Boundary Thrust, active faults, and Main Himalayan Thrust.作者: 侵略者 時間: 2025-3-29 12:20
Jiing-Yih Lai,Zhang Yuanzhi,Y. Z. Zhang of Taplejung window; Lesser Himalayan rocks of Tribeni–Dharan–Dhankuta area; Leoti Group of rocks, and overlying Bhendetar Group; Chimra Thrust separating Bhendetar Group from overlying Phongsawa Group; Barahakshetra Group and Gondwanas; Lesser Himalayan rocks of Mechi transect recording gradual increase in metamorphic grade作者: HARD 時間: 2025-3-29 18:21
Southeast Himalaya and Adjacent Indian Peninsulaines: Darjeeling Gneiss, lime-silicates, pegmatites, and basic sills; inverted metamorphism; proposition of huge recumbent fold; folded Tethyan rocks; interrupted Siwalik belt; south-tilted alluvial terraces; frontal anticline作者: yohimbine 時間: 2025-3-29 21:28 作者: 身心疲憊 時間: 2025-3-30 00:30 作者: 夾死提手勢 時間: 2025-3-30 07:57
Introductionon of Nepal Himalaya by previous investigators; division of Nepal Himalaya into six longitudinal belts and six transverse regions; main characteristics of six transverse regions; summary of 36 chapters of book.作者: notification 時間: 2025-3-30 12:09 作者: 瘙癢 時間: 2025-3-30 12:48
2364-6438 geological maps and cross-sections.New geological observatio.This book addresses the geology of the entire Himalayan range in Nepal, i.e., from the Gangetic plain in the south to the Tethyan zone in the north. Without a comprehensive look at the various Himalayan zones, it is practically impossible 作者: relieve 時間: 2025-3-30 18:03
https://doi.org/10.1057/9781137344250on of Nepal Himalaya by previous investigators; division of Nepal Himalaya into six longitudinal belts and six transverse regions; main characteristics of six transverse regions; summary of 36 chapters of book.
