標(biāo)題: Titlebook: Structural Geology and Tectonics Field Guidebook — Volume 1; Soumyajit Mukherjee Book 2021 Springer Nature Switzerland AG 2021 Field Guide [打印本頁] 作者: 領(lǐng)口 時(shí)間: 2025-3-21 18:03
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書目名稱Structural Geology and Tectonics Field Guidebook — Volume 1讀者反饋學(xué)科排名
作者: jumble 時(shí)間: 2025-3-21 22:05 作者: 一起 時(shí)間: 2025-3-22 01:12
Shilpa Patil Pillai,Vivek S. Kaleion, we will make one further restrictions on the quantifiers to be considered in this sec- tion: we will assume that they obey EXT. This was defined in chapter 3; here we repeat definition 3.2.5 simplified to the (1, 1) type:.. (EXT) A quantifier Q of type (1, 1) follows EXT if for all ., ..,.. ? .作者: 憤世嫉俗者 時(shí)間: 2025-3-22 05:19 作者: 煤渣 時(shí)間: 2025-3-22 12:05
Rajkumar Ghosh,Soumyajit Mukherjeems in complex form, based on linear interpolation (or two-sided prediction) theory as a generalization of linear prediction theory. The conventionally adopted QRD-LSL prediction algorithm can be derived directly from the QRD-LSL interpolation algorithm and then extended to solve the joint process es作者: 凹室 時(shí)間: 2025-3-22 13:51
Mohit Kumar Puniya,Soumyajit Mukherjeems in complex form, based on linear interpolation (or two-sided prediction) theory as a generalization of linear prediction theory. The conventionally adopted QRD-LSL prediction algorithm can be derived directly from the QRD-LSL interpolation algorithm and then extended to solve the joint process es作者: 煩憂 時(shí)間: 2025-3-22 18:15 作者: Noisome 時(shí)間: 2025-3-22 21:20 作者: flaunt 時(shí)間: 2025-3-23 04:16 作者: Compassionate 時(shí)間: 2025-3-23 06:24 作者: Adulterate 時(shí)間: 2025-3-23 11:49
Sukanta Goswami,P. K. Upadhyay,V. Natarajaners and a good overview for existing specialists.Includes suThe attraction of quantum computation and quantum communica- tion theory and experiments hes in the fact that we engineer both them themselves and the quantum systems they treat. This approach has turned out to be very resiUent. Driven by t作者: Inclement 時(shí)間: 2025-3-23 15:26 作者: 安裝 時(shí)間: 2025-3-23 18:13
https://doi.org/10.1007/978-3-030-60143-0Field Guidebook; Structural Geology; Tectonics; Deformation Structures; Stratigraphy; hydrogeology作者: 取之不竭 時(shí)間: 2025-3-24 00:46 作者: 反省 時(shí)間: 2025-3-24 03:46
Geological Field Guide: Malvan (Maharashtra, India),We present a geological field guide for a lesser known location to (Indian) geologists from Maharashtra (India): Malvan. Geomorphological and structural geology exercises have been explained, and a few results have been shown from the 2016 field report of the third author.作者: 沉積物 時(shí)間: 2025-3-24 08:52 作者: Receive 時(shí)間: 2025-3-24 12:45
Review of the Geometric Model Parameters of the Main Himalayan Thrust,Central, and other portions of the Himalaya. It is expected that when a fieldworker works on the Main Frontal Thrust (MFT), these compiled data will be useful in generating models involving subsurface and surface data sets.作者: 令人發(fā)膩 時(shí)間: 2025-3-24 16:33
978-3-030-60142-3Springer Nature Switzerland AG 2021作者: KEGEL 時(shí)間: 2025-3-24 22:01
Structural Geology and Tectonics Field Guidebook — Volume 1978-3-030-60143-0Series ISSN 2197-9545 Series E-ISSN 2197-9553 作者: 先鋒派 時(shí)間: 2025-3-24 23:28
A Field Guide to the Champaner Region, Southern Aravalli Mountain Belt (SAMB), Gujarat, Western Indvided into 4 traverses, from the Champaner region of Western India, with an aim to cater various geological disciples such as structural geology, igneous and metamorphic petrology, basics of stratigraphy, etc.作者: harpsichord 時(shí)間: 2025-3-25 06:09
,Strain Softening in a Continental Shear Zone: A Field Guide to the Excursion in the Ferriere-Molliè the syn-shearing exhumation and retro-metamorphism. The aim of the field trip is to visit some key outcrops that allow to recognize such evolution and to observe the main features of the Ferriere-Mollières Shear Zone that can be regarded as a good example of a strain?softening shear zone in the continental crust.作者: 問到了燒瓶 時(shí)間: 2025-3-25 09:26 作者: Gastric 時(shí)間: 2025-3-25 12:29 作者: 纖細(xì) 時(shí)間: 2025-3-25 18:34
,Tectonics and Channel Morpho-Hydrology—A Quantitative Discussion Based on Secondary Data and Field th East foreland basin of North Bengal, the Singbhum Shear Zone (SSZ) and the Janauri–Chandigarh anticline. Analyses of morpho-hydrological parameters are also applicable through statistical techniques such as Analytical Hierarchy Process (AHP) and the Technique for Order of Preference is done by Similarity Ideal Solution (TOPSIS).作者: CLOUT 時(shí)間: 2025-3-25 22:03 作者: Venules 時(shí)間: 2025-3-26 00:46 作者: 繼承人 時(shí)間: 2025-3-26 07:24 作者: 平庸的人或物 時(shí)間: 2025-3-26 09:17
,Strain Softening in a Continental Shear Zone: A Field Guide to the Excursion in the Ferriere-Molliè In this guide, we describe a two-day field trip in the Argentera External Crystalline Massif (Western Alps). The Massif is cross-cut by the NW-SE oriented Ferriere-Mollières Shear Zone, a spectacular example of a nearly 25-km-long regional transpressive zone with a maximum thickness of 2?km and a c作者: 多產(chǎn)子 時(shí)間: 2025-3-26 15:54
The Geometry and Kinematics of the Southwestern Termination of the Pyrenees: A Field Guide to the Shree main stops with panoramic views. We pursue to emphasize some outstanding characteristics of this structure: (A) the large-scale progressive (laterally angular) unconformity that crops out in its southern flank, fully records its folding kinematics and witnesses for two distinct deformation peri作者: malapropism 時(shí)間: 2025-3-26 18:28 作者: 含水層 時(shí)間: 2025-3-26 21:30
The Southern Iberian Shear Zone (SW Spain): Inclined Transpression Related to Variscan Oblique Conv northern central Huelva province (SW Spain). This boundary forms part of the Rheic Ocean suture, one of the major sutures of the Variscan belt in Europe, and was formed by the Paleozoic sinistral oblique convergence and collision between Avalonia and Armorica in SW Iberia. Strain was partitioned be作者: 手銬 時(shí)間: 2025-3-27 02:58
A Field Guide to the Spectacular Salt Mines of the Transylvanian Basin and Romanian Carpathians,lds, boudinage, etc. Salt structures are themselves valuable as a resource but are also often associated with significant hydrocarbon accumulations, as well as valuable as storage sites. While significant progress has been made to imagine the external geometry of salt bodies, especially using 3D sei作者: 射手座 時(shí)間: 2025-3-27 08:54 作者: Preserve 時(shí)間: 2025-3-27 11:30
Field Guide to RODS in the Pireneus Syntaxis, Central Brazil,formation. Quartz rods are one of the most eye-catching linear structures in deformed rocks. Despite relatively rare, rods are described in several places worldwide. Wherever rods occur, they are promptly noticed. Rods form a conspicuous coarse lineation, frequently highly contrasting with the surro作者: 玷污 時(shí)間: 2025-3-27 14:26
,Low Baric Metamorphic Belts in the Northern Tip of the Arabian–Nubian Shield: Selected Examples froy post-orogenic rift-related plutonism. However, it has proven correct that magmatic activity at any stage of the orogen can provide the required temperature to initiate and drive the metamorphism. The Arabian–Nubian Shield (ANS), the northern part of the Neoproterozoic East African Orogen (EAO), is作者: forthy 時(shí)間: 2025-3-27 18:13 作者: 委屈 時(shí)間: 2025-3-28 01:41 作者: Fulsome 時(shí)間: 2025-3-28 03:14
Tectonic Framework of Northern Pakistan from Himalaya to Karakoram,s and magmatism form by subduction of a denser oceanic crust beneath a continental crust. Ocean–ocean convergence associated plutonic and volcanic magmatism culminated into an island arc. Complete subduction of an intervening oceanic crust leads to collision orogenic belts and suture zones. Suture z作者: 意外 時(shí)間: 2025-3-28 10:18
,Structural Geology Along the Nainital–Pangot Road (Kilbari Section), Nainital Lesser Himalaya (Uttaults, from the Nainital–Pangot road. We expect geological trainers will find this track interesting and will conduct tectonic fieldwork here. The Department of Geology (Kumaun University) is located close to this study area, and it will be very easy to bring the B.Sc. and M.Sc. students from this de作者: 束縛 時(shí)間: 2025-3-28 14:04
Geology, Structural, Metamorphic and Mineralization Studies Along the Mandi-Kullu-Manali-Rohtang Sed to showcase the structural geological marvels of the Mandi-Kullu-Manali section along the Beas River valley from the Main Boundary Thrust (MBT) to the South Tibetan Detachment System (STDS). This dip-section along the road provides an excellent opportunity to study the structural imprints of MBT, 作者: 有角 時(shí)間: 2025-3-28 14:58 作者: aspersion 時(shí)間: 2025-3-28 22:09 作者: creditor 時(shí)間: 2025-3-29 01:36 作者: facilitate 時(shí)間: 2025-3-29 06:48
Book 2021important in the last few years from both academic and industrial perspectives. This book also works as a resource material for batches of students or geological survey professional undergoing training as parts of their course curriculum. Industry persons, on the other hand, can get a first-hand ide作者: 木訥 時(shí)間: 2025-3-29 09:25 作者: 外露 時(shí)間: 2025-3-29 14:25 作者: 獨(dú)白 時(shí)間: 2025-3-29 16:45
Manuel Díaz-Azpiroz,Carlos Fernándezsing completely different approaches, and there thus seems to be a natural agreement about what is a reasonable level of granularity of topological relations, there is no indication so far that these relations are also interesting from a cognitive point of view.作者: confide 時(shí)間: 2025-3-29 21:13 作者: Decline 時(shí)間: 2025-3-30 01:00
Shilpa Patil Pillai,Vivek S. Kalesets are finite. Thus, we restrict ourselves to finite quan- tifiers, those where all arguments are finite sets. Hence, matters of cardinality can be seen as simply arithmetic predicates on natural numbers. To define quantifiers, then, we can give properties on natural numbers.作者: 運(yùn)動(dòng)吧 時(shí)間: 2025-3-30 05:34 作者: 情愛 時(shí)間: 2025-3-30 10:18
Rajkumar Ghosh,Soumyajit Mukherjees at each time step. Therefore, linear interpolation theory may provide a bridge between lattice filters and transversal filters. The chapter is organized as follows. Section 5.1 presents the fundamentals of QRD-LSL algorithms. The LSL interpolator and the LSL predictor are briefly presented in Sect作者: 無王時(shí)期, 時(shí)間: 2025-3-30 16:16 作者: 遺棄 時(shí)間: 2025-3-30 17:13 作者: 解凍 時(shí)間: 2025-3-30 23:45 作者: FOLLY 時(shí)間: 2025-3-31 02:50
Ashwin Pundalik,Shiba Nikalje,Arnav Samant,Hrishikesh Samanttically impossible to completely distinguish photon Bell states, three new approaches appeared: hyperentanglement, the use of continuous variables, and the Knill-Laflamme-Milburn proposal. There are many more such examples. What facilitated all these breakthroughs is the fact that at the present sta作者: ABYSS 時(shí)間: 2025-3-31 05:41 作者: exophthalmos 時(shí)間: 2025-3-31 09:30 作者: 太空 時(shí)間: 2025-3-31 14:08
Miocene-Quaternary Strain Partitioning and Relief Segmentation Along the Arcuate Betic Fold-and-Thrpresentative area of the inner FTB characterized by a set of parallel mountain ranges enclosing the Ronda intermontane basin. In this area, the topography is conditioned by late Miocene to Pliocene km-scale, upright or doubly vergent, NE-SW trending folds and associated reverse faults. These structu作者: Anticoagulants 時(shí)間: 2025-3-31 18:57 作者: 勤勉 時(shí)間: 2025-3-31 23:25
A Field Guide to the Spectacular Salt Mines of the Transylvanian Basin and Romanian Carpathians, especially because most of the salt mines have been converted into public treatment facilities. The walls of the galleries have been cleaned, polished and well lighted, offering unique 3D exposures which can be used to observe and map in detail the deformation of these salt domes. In this field-tri作者: 使入迷 時(shí)間: 2025-4-1 02:02
Field Guide to RODS in the Pireneus Syntaxis, Central Brazil,onfused to mullions, boudins and pencil structures, since these are also elongated and rounded structures. But striking differences in their geometry and genesis can be used to distinguish between them. In this guide, the various definitions of rods and how they distinguish from other structures are作者: Irascible 時(shí)間: 2025-4-1 06:28
Tectonic Framework of Northern Pakistan from Himalaya to Karakoram,to examine Andean/Cordilleran, Island Arc and continent–continent orogenic belts and diverse geological processes associated with their formation. In this chapter, we communicate to the readers to canvas the Sub-Himalaya, Greater Himalaya, remnants of the southern and northern Neo–Tethys that have b作者: 男學(xué)院 時(shí)間: 2025-4-1 13:44
Geology, Structural, Metamorphic and Mineralization Studies Along the Mandi-Kullu-Manali-Rohtang Seeets including Chail and Jutogh groups and intrusive Paleozoic granites, (iii) High-grade crystallines and migmatites of the Higher Himalayan Crystalline (HHC) including intrusive Paleozoic leucogranites, (iv) Tethyan Himalayan Sequence (THS). Based on our field, structural and metamorphic observati作者: BOON 時(shí)間: 2025-4-1 16:35 作者: frivolous 時(shí)間: 2025-4-1 19:44
