找回密碼
 To register

QQ登錄

只需一步,快速開始

掃一掃,訪問微社區(qū)

打印 上一主題 下一主題

Titlebook: Geodynamics of the Indian Plate; Evolutionary Perspec Neal Gupta,Sampat K. Tandon Book 2020 Springer Nature Switzerland AG 2020 Indian Ocea

[復(fù)制鏈接]
樓主: Thoracic
21#
發(fā)表于 2025-3-25 05:12:54 | 只看該作者
22#
發(fā)表于 2025-3-25 08:17:09 | 只看該作者
https://doi.org/10.1007/978-3-662-41571-9ub-Himalaya zone was developed in front of the rising Himalaya. It is bounded between the Main Boundary Thrust (MBT) and the Himalayan Frontal Thrust (HFT). The Himalayan Frontal Fault zone encompasses the frontal anticlines, dun?(intermontane basins) and hinterland fold-thrusts. The tectonic geomor
23#
發(fā)表于 2025-3-25 15:42:09 | 只看該作者
https://doi.org/10.1007/978-3-7091-7934-5n the past few decades, research was focused on the assessment of the relative importance of various forcing factors that governed sediment accumulation patterns in time and space in the Ganga Plains, which when considered together explain the geomorphic diversity within the basin. The Ganga basin i
24#
發(fā)表于 2025-3-25 17:16:44 | 只看該作者
25#
發(fā)表于 2025-3-25 20:10:47 | 只看該作者
Elektrische Widerstandspyrometer,ue climatic regimes. The southwest monsoon season from June to September (JJAS) is associated with drought and flood, active and break cycle of monsoon and heavy rainfall over different parts of the country. Similarly, October to December (OND) season is associated with northeast monsoon season over
26#
發(fā)表于 2025-3-26 03:48:27 | 只看該作者
Neal Gupta,Sampat K. TandonMaximizes understanding on all the major geological provinces of the Indian Plate.Tracks and examines the evolution of the Indian landmass through various supercontinent assemblies.Delves into aspects
27#
發(fā)表于 2025-3-26 04:25:58 | 只看該作者
https://doi.org/10.1007/978-3-030-15989-4Indian Ocean dynamics; Precambrian Cratons of India; Indian stratigraphic record; Proterozoic sedimenta
28#
發(fā)表于 2025-3-26 11:37:23 | 只看該作者
Introduction to Geodynamics of the Indian Plate: Evolutionary Perspectives,icratonic basins along the eastern and western margins of India—formed in the Paleozoic-Mesozoic. In the Cenozoic, the Himalayas and its foreland were initiated and continued to develop in response to the northward migration of the Indian Plate, and its subduction beneath the Eurasian Plate and coll
29#
發(fā)表于 2025-3-26 15:47:44 | 只看該作者
30#
發(fā)表于 2025-3-26 20:18:40 | 只看該作者
 關(guān)于派博傳思  派博傳思旗下網(wǎng)站  友情鏈接
派博傳思介紹 公司地理位置 論文服務(wù)流程 影響因子官網(wǎng) 吾愛論文網(wǎng) 大講堂 北京大學 Oxford Uni. Harvard Uni.
發(fā)展歷史沿革 期刊點評 投稿經(jīng)驗總結(jié) SCIENCEGARD IMPACTFACTOR 派博系數(shù) 清華大學 Yale Uni. Stanford Uni.
QQ|Archiver|手機版|小黑屋| 派博傳思國際 ( 京公網(wǎng)安備110108008328) GMT+8, 2025-10-6 21:53
Copyright © 2001-2015 派博傳思   京公網(wǎng)安備110108008328 版權(quán)所有 All rights reserved
快速回復(fù) 返回頂部 返回列表
宜章县| 乐平市| 江安县| 久治县| 孝昌县| 蛟河市| 阿拉善左旗| 四平市| 冷水江市| 故城县| 临猗县| 白玉县| 大名县| 伊春市| 扶风县| 双鸭山市| 武宁县| 昌江| 庄河市| 黄浦区| 灵台县| 张家界市| 抚松县| 罗平县| 沈丘县| 高雄市| 当阳市| 沁源县| 确山县| 拜城县| 舟山市| 青神县| 无锡市| 海南省| 五大连池市| 桂东县| 青海省| 闻喜县| 峡江县| 屯昌县| 浦县|