標(biāo)題: Titlebook: Cave and Karst Systems of Hungary; Márton Veress,Szabolcs Leél-?ssy Book 2022 Springer Nature Switzerland AG 2022 Hungarian karst areas.Ka [打印本頁(yè)] 作者: 老鼠系領(lǐng)帶 時(shí)間: 2025-3-21 17:33
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書目名稱Cave and Karst Systems of Hungary讀者反饋學(xué)科排名
作者: POLYP 時(shí)間: 2025-3-21 22:01
,Vertiefungsübungen zu OP-Schaltungen,orphic evolution of karst surfaces, processes and phenomena related to epigenetic valley development, surface karst features, and caves (cold-water caves and warm-water caves are discussed separately).作者: coltish 時(shí)間: 2025-3-22 01:26 作者: 輕快走過 時(shí)間: 2025-3-22 06:42 作者: Gossamer 時(shí)間: 2025-3-22 09:56
An Interpretation of Karstification and Karst Processes by Hungarian Researchers,orphic evolution of karst surfaces, processes and phenomena related to epigenetic valley development, surface karst features, and caves (cold-water caves and warm-water caves are discussed separately).作者: Liberate 時(shí)間: 2025-3-22 14:38
The Surface Morphology of Karsts in Hungary,h history, the general description of their karstification, the morphometric study of the karst features belonging to their area, the morphology, morphological environment, genetics, and development of karst features.作者: Liberate 時(shí)間: 2025-3-22 20:58
Sedimentologic, Taphonomic Processes and Paleontological Values of Hungarian Caves,ical paleontologic and/or archaeologic remains, the age and biochronologic positions. Most of the illustrations have historical value, first published here. The reference is containing the basic works, the most important priority papers and the current publications.作者: 氣候 時(shí)間: 2025-3-22 22:31
2364-4591 cludes a separate chapter which deals with the history of Hungarian karst and cave research. Another chapter deals with theories that were made during Hungarian karst researches. .978-3-030-92962-6978-3-030-92960-2Series ISSN 2364-4591 Series E-ISSN 2364-4605 作者: 啪心兒跳動(dòng) 時(shí)間: 2025-3-23 01:40
https://doi.org/10.1007/978-3-8348-9437-3racteristic feature is also present, but it is less widespread and concealed karstification started in the Würmian or earlier, but its beginning is also different on the blocks belonging to various types.作者: conifer 時(shí)間: 2025-3-23 08:14
The Geomorphic Evolution of Karsts and Karstic Surfaces,racteristic feature is also present, but it is less widespread and concealed karstification started in the Würmian or earlier, but its beginning is also different on the blocks belonging to various types.作者: 有角 時(shí)間: 2025-3-23 12:01 作者: larder 時(shí)間: 2025-3-23 15:34 作者: 行為 時(shí)間: 2025-3-23 18:06
Book 2022 geology, their paleokarst, their hydrology, their surface and subsurface morphology (more significant caves are classified according to karst areas and their morphology and development is described), ecology and flora and fauna..This book also includes a separate chapter which deals with the histor作者: anaphylaxis 時(shí)間: 2025-3-23 23:28 作者: 興奮過度 時(shí)間: 2025-3-24 02:38
Book 2022nd their morphology and development is described), ecology and flora and fauna..This book also includes a separate chapter which deals with the history of Hungarian karst and cave research. Another chapter deals with theories that were made during Hungarian karst researches. .作者: interlude 時(shí)間: 2025-3-24 09:44 作者: 革新 時(shí)間: 2025-3-24 14:42 作者: Confound 時(shí)間: 2025-3-24 16:44 作者: 做事過頭 時(shí)間: 2025-3-24 20:24
Cave and Karst Systems of Hungary978-3-030-92960-2Series ISSN 2364-4591 Series E-ISSN 2364-4605 作者: Mendicant 時(shí)間: 2025-3-25 00:16
,Erweiterter Koh?renzmatrizen-Kalkül,onsider the most significant. We present the general genetic grouping of the caves and then characterize the major caves of the two mountains according to a system of criteria. Such as their geographical location, their host rock, the genetics and the speleothem of the caves.作者: 機(jī)械 時(shí)間: 2025-3-25 06:07 作者: 能夠支付 時(shí)間: 2025-3-25 10:02
Optimierungsaufgaben im Banachraum,The general characteristics of the karsts in Hungary are surveyed. The main properties of karst areas are described: their position, elevation, expansion, division, geomorphology and karst types.作者: 觀察 時(shí)間: 2025-3-25 12:44
A General Description of Karsts in Hungary,The general characteristics of the karsts in Hungary are surveyed. The main properties of karst areas are described: their position, elevation, expansion, division, geomorphology and karst types.作者: abnegate 時(shí)間: 2025-3-25 19:01 作者: 縫紉 時(shí)間: 2025-3-25 22:36
978-3-030-92962-6Springer Nature Switzerland AG 2022作者: Pessary 時(shí)間: 2025-3-26 02:04 作者: 繞著哥哥問 時(shí)間: 2025-3-26 06:31 作者: SIT 時(shí)間: 2025-3-26 08:49
,Vertiefungsübungen zu OP-Schaltungen, stages of their evolution (Sect. .. Budai T. and Kercsmár Zs.). Geological features of the mountain ranges are summarized according to their tectonic and lithostratigraphic characteristics. The relationship between the stratigraphic units is shown in pre-Cenozoic and Cenozoic lithostratigraphic cha作者: 前奏曲 時(shí)間: 2025-3-26 14:55 作者: 牲畜欄 時(shí)間: 2025-3-26 17:48
https://doi.org/10.1007/978-3-8348-9437-3flow framework which is the adaptation of groundwater flow systems to carbonate regions and, thus, a novel approach in karst hydrogeology studies. Accordingly, a solid but comprehensive overview of the hydrogeologic environment (topography, climate, and geology), groundwater flow patterns and proces作者: 浮夸 時(shí)間: 2025-3-26 21:12 作者: Rebate 時(shí)間: 2025-3-27 01:41
Klassifizierung optischer Netzwerke,n, the Vértes Plateau, the Gerecse Region, the Buda Hills, the Pilis Mountains, and the Western Mecsek Karst. Their description involves their research history, the general description of their karstification, the morphometric study of the karst features belonging to their area, the morphology, morp作者: 制定 時(shí)間: 2025-3-27 05:44
,Erweiterter Koh?renzmatrizen-Kalkül,ases and visualizations, but the analytical capabilities of GIS were also increasingly applied in karst research. Data collection has been revolutionized by continuously evolving remote sensing methods (e.g. LiDAR). GIS became crucial in doline morphometry, thus in this chapter, we present a detaile作者: WATER 時(shí)間: 2025-3-27 10:22
Klassifizierung optischer Netzwerke,e of well-developed plateau karsts in the humid temperate climate zone. Numerous surface and subsurface landforms (285 caves) were created by the intense karstification of Triassic limestones. The compound multi-phase evolution of karst from the Late Cretaceous to the present is recorded in the morp作者: 世俗 時(shí)間: 2025-3-27 16:55
Klassifizierung optischer Netzwerke,ed for completeness (since the Bükk Mountains is the richest in caves in Hungary). By the selection, we aimed to include the most significant caves based on the most representative cave types and sizes, speleothem or archaeological values of the mountains. We review the genetic types of the caves in作者: 胰臟 時(shí)間: 2025-3-27 19:42
Klassifizierung optischer Netzwerke,d marl, during the Middle and Late Pleistocene. Recently we have 60?km of known cave passages mapped, chiefly in the Rózsadomb (Rose Hill) part of the city. Every cave was discovered by accident (stone quarrying, digging basements, trenching for gas and water pipes, canalization, etc.). These caves 作者: 討厭 時(shí)間: 2025-3-27 23:40 作者: 圍裙 時(shí)間: 2025-3-28 03:02
https://doi.org/10.1007/978-3-8348-9437-3one area. This karst area is similar to the Aggtelek karst and Bükk Mountains (see earlier), basically it is formed by infiltrating cold water and allogenic streams. Besides the rich surface karst forms there are several swallow holes, spring caves and chimneys up to 70?m. This chapter shows the mos作者: anthesis 時(shí)間: 2025-3-28 08:14 作者: 機(jī)警 時(shí)間: 2025-3-28 13:59 作者: 我沒有命令 時(shí)間: 2025-3-28 17:09
https://doi.org/10.1007/978-3-8348-9461-8calities discussed in chronological order contain their locations, history of excavation, important sedimentologic and taphonomic characteristics, typical paleontologic and/or archaeologic remains, the age and biochronologic positions. Most of the illustrations have historical value, first published作者: 總 時(shí)間: 2025-3-28 21:38 作者: aesthetic 時(shí)間: 2025-3-29 02:17
Relationenalgebraische Grundlagen, many endangered, endemic and relict species, indicating past evolutionary dynamics and the alternation of colder and warmer climate periods during the Quaternary. Vegetation structure, species richness, floristic composition and functional traits vary along steep environmental gradients, resulting 作者: Hyperopia 時(shí)間: 2025-3-29 03:35
The Caves of the Southwestern Part of the Transdanubian Mountains (Transdanubian Range),onsider the most significant. We present the general genetic grouping of the caves and then characterize the major caves of the two mountains according to a system of criteria. Such as their geographical location, their host rock, the genetics and the speleothem of the caves.作者: MURKY 時(shí)間: 2025-3-29 07:16 作者: 蘆筍 時(shí)間: 2025-3-29 15:17 作者: AMEND 時(shí)間: 2025-3-29 15:39
Geology of the Karst Terrains in Hungary,pe tectonics), the Bükk and the Szendr? and Uppony Mountains (located in the shear zone of the Mid-Hungarian Mega-unit) (Sects. ., ., .. Less Gy). The later is followed by the geology of the Mecsek and the Villány Mountains in the southern tectonic unit, i.e. the Tisza Mega-unit (Sect. .. Konrád Gy)作者: 相符 時(shí)間: 2025-3-29 22:47
Paleokarst in Hungary, methods and the appropriate understanding of the geological evolution of the area concerned. Selected examples of some early (diagenetic) and late “Alpine”-type paleokarsts are presented and the relevant references discussed.作者: AWL 時(shí)間: 2025-3-30 00:14 作者: CEDE 時(shí)間: 2025-3-30 06:37
GIS Research of Karst Terrains in Hungary,also provided here. During the last centuries, Hungarian karst terrains have undergone significant landscape changes. Based on earlier series of military maps, satellite images and other databases (e.g. CORINE), these landscape changes have been studied by several authors using GIS methodology. More作者: sclera 時(shí)間: 2025-3-30 08:27
,The Caves of Aggtelek Karst, Szalonna Karst and Rudabánya Mountains,cave system is an excellent example of a fluvially modelled ‘ideal watertable cave’. Several multi-level caves were formed by allogenic sinking streams at the edge of karst plateaus or along traverse valleys. The Baradla–Domica cave system hosts more than 500 animal species and played an important r作者: Infiltrate 時(shí)間: 2025-3-30 13:29
The Caves of the Northeastern Part of the Transdanubian Mountains, water passages in Molnár János Cave. József-hegy Cave, Citadella Crystal Cave and Királylaki Cave are accessible for research projects only. There are fewer, but very interesting, caves in the Triassic limestone of the Pilis Hills. The intensively investigated Ariadne Cave System is now nearly 20?k作者: mortgage 時(shí)間: 2025-3-30 20:37
Monitoring and Geochemical Investigations of Caves in Hungary: Implications for Climatological, Hydnstruct past climate and environmental fluctuations. In addition, the equations that best describe the carbonate-water oxygen isotope fractionation and best reflect the temperature dependence of the isotopic composition of precipitations were identified for paleotemperature reconstruction. The inves作者: hyperuricemia 時(shí)間: 2025-3-30 23:21
Age, Depositional Environment, and Geochemistry of Freshwater Carbonates (Travertine, Tufa) from Hu oil reservoir rocks. Furthermore, the recent deposits can be used for the calibration of the oxygen- and clumped isotope paleothermometers. The aim of this chapter is to provide a short review of the most important Hungarian travertine and tufa deposits including the achievements of most recent res作者: 確定的事 時(shí)間: 2025-3-31 03:52
The Vegetation of Karsts in Hungary, and this trend will probably continue in coming decades. The capacity of karstic refugia to buffer against the negative effects of climate oscillations on vegetation is likely to be exceeded if the current management practices will remain unchanged. In this chapter, the phytogeography, community st作者: Mosaic 時(shí)間: 2025-3-31 06:47
https://doi.org/10.1007/978-3-8348-9357-4Hill. The work of Hungarian cave researchers contributed to solving the problems of several special karstic phenomena (e.g. the formation of helictites, the effect of tidal phenomena on the discharge of karst springs). Furthermore, the contribution of Hungarian cave researchers was also important in作者: gratify 時(shí)間: 2025-3-31 12:25 作者: arthroscopy 時(shí)間: 2025-3-31 14:58 作者: ULCER 時(shí)間: 2025-3-31 17:32
https://doi.org/10.1007/978-3-8348-9437-3es, mixing of meteoric and basinal and waters of local, intermediate and regional groundwater flow systems and potential locations of epigene and hypogene speleogenesis can be revealed and explained. The Hungarian karst areas reflect different properties but there are similarities regarding their hy作者: 有惡臭 時(shí)間: 2025-4-1 00:15
,Erweiterter Koh?renzmatrizen-Kalkül,also provided here. During the last centuries, Hungarian karst terrains have undergone significant landscape changes. Based on earlier series of military maps, satellite images and other databases (e.g. CORINE), these landscape changes have been studied by several authors using GIS methodology. More作者: 歡笑 時(shí)間: 2025-4-1 01:53 作者: 商品 時(shí)間: 2025-4-1 09:56 作者: 脫離 時(shí)間: 2025-4-1 14:10 作者: Asseverate 時(shí)間: 2025-4-1 17:18 作者: coalition 時(shí)間: 2025-4-1 20:56 作者: 不妥協(xié) 時(shí)間: 2025-4-1 22:57
History of Karst and Cave Research in Hungary,xplicitly dealt with limestone mountains including their spectacular large cave?entrances and their famous gorges. The caves of Hungary are widely known in the world based on their natural, cultural and historical values as well as their role in scientific research, despite the fact that there are n
