標(biāo)題: Titlebook: Intracontinental Fold Belts; Case Studies in the Henno Martin,Franz Wolfgang Eder Conference proceedings 1983 Springer-Verlag Berlin Heide [打印本頁] 作者: Maculate 時(shí)間: 2025-3-21 17:02
書目名稱Intracontinental Fold Belts影響因子(影響力)
作者: seroma 時(shí)間: 2025-3-21 20:55
H. Martin,H.-J. Behrhe waveguide with open ends and waveguides from the focusing mirrors. In particular, we describe the class of open cylindrical coaxial resonators. Based on these, systems with an extremely rare spectrum of fundamental frequencies were developed (the Nefyodov–Rossiyskiy effect). This resonator can se作者: Trochlea 時(shí)間: 2025-3-22 03:20 作者: 的’ 時(shí)間: 2025-3-22 07:55
F. W. Eder,W. Engel,W. Franke,P. M. Sadler the past two decades electromagnetic field computations have received a big impulse by the large availability of digital computers with better and better performances in speed and capacity. Many various methods have been developed but not all of them appear convenient enough for practical engineeri作者: 脫落 時(shí)間: 2025-3-22 11:05 作者: Barrister 時(shí)間: 2025-3-22 13:00
K. H. Wedepohl,K. Meyer,G. K. Mueckeelectromagnetic field outside a moving body can also be created by static charges which are always present on the surface of the body due to inhomogeneities, or due to a bias voltage. This electromagnetic field produces electrostatic friction which can be significantly enhanced if on the surface of 作者: endarterectomy 時(shí)間: 2025-3-22 19:29
W. Engel,W. Franke,C. Grote,K. Weber,H. Ahrendt,F. W. Eder Erkol, B. Isildak, M. Oka, T.T. Takahashi, Physics Letters B726 (2013) 703-709, K.U. Can, G. Erkol, B. Isildak, M. Oka, T.T. Takahashi, Journal of High Energy Physics (JHEP) 05, 125 (2014) and K.U. Can, G. Erkol, M. Oka, T.T. Takahashi, Physical Review D 92, 114515 (2015).作者: Madrigal 時(shí)間: 2025-3-22 22:29 作者: 調(diào)整 時(shí)間: 2025-3-23 03:34 作者: delta-waves 時(shí)間: 2025-3-23 07:42
H. Wilhelm,U. Schmuckerknowledge provides useful pointers towards the design of efficient collectors. Also, at high-power concentration levels, optical reflectors are subject to thermal effects and the thermodynamics required to comprehend the relevant phenomena are presented in Sect.?..作者: Macronutrients 時(shí)間: 2025-3-23 12:35 作者: 思鄉(xiāng)病 時(shí)間: 2025-3-23 16:57 作者: Conjuction 時(shí)間: 2025-3-23 21:46 作者: 巡回 時(shí)間: 2025-3-24 01:41 作者: 謙虛的人 時(shí)間: 2025-3-24 03:34
F. Langenstrassenslotted and edge-dielectric transmission lines are described.?A large number of Mathcad programs for illustration of field patterns and its properties in different guiding structures are provided. The material 978-3-030-08114-0978-3-319-90847-2Series ISSN 2524-4345 Series E-ISSN 2524-4353 作者: 小隔間 時(shí)間: 2025-3-24 08:04 作者: 破裂 時(shí)間: 2025-3-24 10:58
W. Kasig,H. Wildercy makers and anyone else interested in a deeper understanding of the health effects of electromagnetic fields. Intended to serve a broad readership, everyone will approach it according to their respective leve978-2-8178-0362-3978-2-8178-0363-0作者: Juvenile 時(shí)間: 2025-3-24 16:42 作者: indubitable 時(shí)間: 2025-3-24 20:30 作者: Suggestions 時(shí)間: 2025-3-25 02:58 作者: Essential 時(shí)間: 2025-3-25 04:19
The Mineral Composition of Rhenohercynian Flysch Sediments and Its Tectonic Significance(approx. 1 mm)..As it was already known from earlier thin-section studies, the content of feldspar decreases from about 30% (Devonian through Lower Carboniferous III-alpha) to about 10% (in the Upper Carboniferous). The bulk of feldspar is present in the form of albite, which probably originated fro作者: 柳樹；枯黃 時(shí)間: 2025-3-25 11:02
The Sedimentary Development of the Western Rheinisches Schiefergebirge and the Ardennes (Germany/BelAachen, Vesdre Massif)..Nowadays the evaporites lie as sulfates under the Dinant Nappe which can be traced from northern France to Aachen. Its northern boundary is marked by the Midi Overthrust (“Faille du Midi”)..The formation of the thick foredeep sediments during the Namurian and Westphalian mean作者: fatty-acids 時(shí)間: 2025-3-25 14:27 作者: 流逝 時(shí)間: 2025-3-25 19:45 作者: 認(rèn)為 時(shí)間: 2025-3-25 21:13 作者: grenade 時(shí)間: 2025-3-26 01:31
Nappe Tectonics in the Southeastern Part of the Rheinisches Schiefergebirgef the greywacke area, are interpreted as allochthonous rafts at the base of the nappe. These are: phyllonitic sediments (much stronger metamorphosed than the surrounding units, with older K/Ar ages of mica), strongly sheared tectonic lenses of spilite (with the trace-element configuration of ocean-r作者: Devastate 時(shí)間: 2025-3-26 05:39 作者: Detonate 時(shí)間: 2025-3-26 10:59 作者: enmesh 時(shí)間: 2025-3-26 14:28
Experimental Study of Subfluence Tectonics in the Rheinische Schiefergebirge cool and therefore stable continental lithosphere. In areas where incipient folding and thrusting are accompanied by isostatic movement, possibly due to higher heatflow, synclinal structures become strongly amplified during deformation and the development of synclinal structures may predominate.作者: MODE 時(shí)間: 2025-3-26 19:39 作者: GRIN 時(shí)間: 2025-3-26 21:54 作者: commonsense 時(shí)間: 2025-3-27 01:52 作者: commensurate 時(shí)間: 2025-3-27 07:04
Flysch, Olistostromes and Nappes in the Harz Mountainsard under the Mid-German Rise..The problem of the original palaeogeographical position of the so-called Hercynian Complex (relative autochthony or allochthony) is still open. Further investigations have to verify which of the two discussed models is applicable.作者: Intuitive 時(shí)間: 2025-3-27 10:45 作者: Fecal-Impaction 時(shí)間: 2025-3-27 13:53
https://doi.org/10.1007/978-3-642-69124-9Gebirge; Sediment; Sedimentation; Turbidite; environment; evolution; geochemistry; geography; geology; geophy作者: 弓箭 時(shí)間: 2025-3-27 19:23
Depositional Models for the Carboniferous Flysch of the Eastern Rheinisches Schiefergebirgerapidly evolving, tectonically active troughs during the terminal phase of the development of the orogenic basin. They are derived from and then incorporated into newly influential source terrains. They were deformed at shallow or superficial crustal levels and are primary record of the orogeny.作者: 有機(jī)體 時(shí)間: 2025-3-28 01:30
978-3-642-69126-3Springer-Verlag Berlin Heidelberg 1983作者: 文字 時(shí)間: 2025-3-28 04:12
Overview: 978-3-642-69126-3978-3-642-69124-9作者: 在前面 時(shí)間: 2025-3-28 10:16 作者: 埋伏 時(shí)間: 2025-3-28 12:12
Palaeozoic Sedimentation in the Northern Branch of the Mid-European Variscides — Essay of an Interprnian (and older) orogenies, global hydrographic events, and Variscan A-subduction..Parly Palaeozoic clastics and bimodal volcanics in the Saxothuringian Zone can be referred to a phase of rifting, which compensated for the closure of the Iapetus ocean. The Rhenohercynian Zone was incorporated into t作者: 挫敗 時(shí)間: 2025-3-28 18:20
Neritic Sedimentation of the Lower and Middle Devonian in the Rheinische Schiefergebirge East of theedonian uplands of the Old Fed Continent and in the south by the variable configuration of the Mid?German Crystalline Pise. In the deposition area between, clastic shallow marine sediments accumulated up to 4000 m in thickness by a large delta complex prograding from the north. Relative lithological作者: BRAWL 時(shí)間: 2025-3-28 21:20
“Pelagic” Carbonates in the Variscan Belt — Their Sedimentary and Tectonic Environmentsofacies studies fail to provide unequivocal evidence, the interpretation has to rely mainly on the faunas and on the character of the adjacent facies units. The local abundance of benthonic organisms (including algae) indicates that some pelagic limestones were deposited at shallow depths. Transitio作者: frugal 時(shí)間: 2025-3-29 02:51
Devonian and Carboniferous Limestone-Turbidites of the Rheinisches Schiefergebirge and Their Tectoniion of allochthonous, shallow water, carbonate debris by turbidity currents, which aids in the interpretation of the history of the source regions and of the topography within the basin. The key is always to determine the flow patterns of the turbidity currents. This is rarely possible by reference 作者: 內(nèi)閣 時(shí)間: 2025-3-29 04:38
Depositional Models for the Carboniferous Flysch of the Eastern Rheinisches Schiefergebirgerapidly evolving, tectonically active troughs during the terminal phase of the development of the orogenic basin. They are derived from and then incorporated into newly influential source terrains. They were deformed at shallow or superficial crustal levels and are primary record of the orogeny.作者: 輕率看法 時(shí)間: 2025-3-29 07:20
Flysch, Olistostromes and Nappes in the Harz Mountains Nappe. In the course of the orogeny this nappe has been tectonically subdivided into several units. Whereas the majority of these units suffered relatively strong deformation, the southeastern unit (South Harz/Selke-Unit) was less deformed due to its gravitational emplacement in a relatively late p作者: 男生戴手銬 時(shí)間: 2025-3-29 12:19
The Mineral Composition of Rhenohercynian Flysch Sediments and Its Tectonic Significance migration of the Devonian through Upper Carboniferous flysch trough. In the Upper Namurian, the flysch grades into coal-bearing molasse. We have analyzed, by infrared-spectroscopy, the composition of the flysch- and the basal molasse rocks, and tried to fit these data into a general tectonic concep作者: ALIBI 時(shí)間: 2025-3-29 16:02
The Sedimentary Development of the Western Rheinisches Schiefergebirge and the Ardennes (Germany/Bel is a distinct interruption of sedimentation between the Caradocian and the Gedinnian..The typical clastic facies of the Rhenish shelf with red sediments from the Old-Red-Continent was succeeded in the Middle Devonian and lower Upper Devonian by carbonates of a wide shelf lagoon. The reefbuilders di作者: 雕鏤 時(shí)間: 2025-3-29 20:31
The Chemical Composition of Sedimentary Deposits in the Rhenohercynian Belt of Central Europeajor and for 15 minor elements. Excepting the abundance of carbonate rocks and metavolcanic materials (spilites, keratophyres, quartz keratophyres) the average composition of the units is remarkably homogeneous throughout the Devonian and Carboniferous. Only the Lower Carboniferous of the SE region 作者: 粗糙 時(shí)間: 2025-3-30 00:14
Chemical Composition and Genetic Relations of Meta-Volcanic Rocks from the Rhenohercynian Belt of Nosent. The climax of volcanism occurred during the Middle Devonian, but activity continued until the Lower Carboniferous (mainly in the Lahn-Dill area)..65 spilites (including picritic and high potassium species) and 16 quartz keratophyres from the Rhenohercynian Belt have been analyzed for the major作者: Proclaim 時(shí)間: 2025-3-30 07:17
Mineral Composition of Pelitic Sediments in the Rhenohercynian Zonelity for exact and rapid quantitative analyses of sedimentary rocks containing illite, chlorite, kaolinite, quartz, feldspars and calcite. Ey their clay mineral/(quartz + feldspar)? ratios and their carbonate contents pelitic rocks were classified into three main types: common shales (215 samples), 作者: 抱狗不敢前 時(shí)間: 2025-3-30 10:33
Nappe Tectonics in the Southeastern Part of the Rheinisches Schiefergebirgeaphic and tectonic findings..The Gie?en Greywacke, a turbidite sequence in the northeastern Lahn Syncline, rests unconformably on Lower through Upper Devonian rocks. Conodonts retrieved from carbonate-cemented greywackes, together with data from the literature, suggest that most (if not all) of the 作者: 食道 時(shí)間: 2025-3-30 16:21
Flysch-Sedimentation: Its Relations to Tectonism in the European Variscidesre in every case directed outward from the ridge..Phenohercynian (northern external Zone): South Portugal, Southwest Fngland-, Pheinisches Schiefergebirge, Harz, with a possible continuation into Moravia (?.S.S.R.). The source-area in Central Furope is the region of the Mid-German Crystalline Pise a作者: 門閂 時(shí)間: 2025-3-30 18:39
Migration of Folding and Metamorphism in the Rheinische Schiefergebirge Deduced from K-Ar and Rb-Sr shifting of flysch sedimentation..In order to get an idea of the time span which the “wave” of folding and metamorphism has needed to pass through the Rheinische Schiefergebirge, isotopic investigations by K-Ar and Rb-Sr methods were carried out. For these measurements the fine mineral fractions <2μ作者: 怒目而視 時(shí)間: 2025-3-31 00:03
Experimental Study of Subfluence Tectonics in the Rheinische Schiefergebirgerelative to the mid-German Crystalline Rise and the boundary condition for isostatic movement following the crustal thickening are the main considerations in the present model experiments..In the model a syncline is formed as the major structure in the supracrust. The weak infracrust also has played作者: 挫敗 時(shí)間: 2025-3-31 02:38 作者: GULLY 時(shí)間: 2025-3-31 08:36
Intracrustal and Subcrustal Thrust-Tectonics at the Northern Margin of the Bohemian Massiflistic concept for the geotectonic developement of these regions..The origin of the Saxothuringian basin can be referred to an Upper Proterozoic to Ordovician rifting process. Metamorphosed sedimentary and basic igneous rocks found along the western margin of the Moldanubian Zone and in the Tepla-Pa作者: Anhydrous 時(shí)間: 2025-3-31 10:32 作者: fatty-streak 時(shí)間: 2025-3-31 14:15
