標題: Titlebook: Cave Exploration in Slovenia; Discovering Over 350 Martin Knez,Tadej Slabe Book 2016 Springer International Publishing Switzerland 2016 Cav [打印本頁] 作者: 導彈 時間: 2025-3-21 17:44
書目名稱Cave Exploration in Slovenia影響因子(影響力)
書目名稱Cave Exploration in Slovenia影響因子(影響力)學科排名
書目名稱Cave Exploration in Slovenia網(wǎng)絡公開度
書目名稱Cave Exploration in Slovenia網(wǎng)絡公開度學科排名
書目名稱Cave Exploration in Slovenia被引頻次
書目名稱Cave Exploration in Slovenia被引頻次學科排名
書目名稱Cave Exploration in Slovenia年度引用
書目名稱Cave Exploration in Slovenia年度引用學科排名
書目名稱Cave Exploration in Slovenia讀者反饋
書目名稱Cave Exploration in Slovenia讀者反饋學科排名
作者: Inexorable 時間: 2025-3-21 21:20 作者: ROOF 時間: 2025-3-22 02:19 作者: WAIL 時間: 2025-3-22 06:28 作者: malign 時間: 2025-3-22 09:22
Cave Exploration in Slovenia978-3-319-21203-6Series ISSN 2364-4591 Series E-ISSN 2364-4605 作者: 平常 時間: 2025-3-22 15:34
Martin Knez,Tadej SlabeFurthers our understanding of cave and karst systems around the world.Includes numerous new findings on karst genesis, hydrology and protection.Bridges the gap between karst research and civil enginee作者: 平常 時間: 2025-3-22 19:13
Cave and Karst Systems of the Worldhttp://image.papertrans.cn/c/image/222671.jpg作者: 古文字學 時間: 2025-3-22 22:04 作者: 鍍金 時間: 2025-3-23 05:02
https://doi.org/10.1007/978-3-8348-9213-3d of old caves, i.e. caves which once had water passing through. Two thirds of these caves were filled with alluvium. Research carried out in these caves augmented knowledge about the development of this part of the Karst region. A cave system extending more than 500 m, which we tried to preserve in作者: evasive 時間: 2025-3-23 08:02 作者: BRUNT 時間: 2025-3-23 11:37 作者: 表示向前 時間: 2025-3-23 17:53 作者: 圣歌 時間: 2025-3-23 18:18 作者: 單調(diào)女 時間: 2025-3-24 01:22
Nichtlineare Optik II: Vierwellenmischung,d flowstone. It became clear during the motorway construction undertaking in Slovenia that unroofed caves constitute a relatively common karst landform. In fact, more common than karstologists had imagined before the karst surface was uncovered through earthworks. The various types of notches occurr作者: 法律的瑕疵 時間: 2025-3-24 03:04 作者: 換話題 時間: 2025-3-24 08:57
Nichtlineare Optik II: Vierwellenmischung,he clastic sediments in some of them have been subjected to in-depth analyses. A sediment analysis has shown that some of these depressions were in fact old caves, filled with fluvial allochthonous sediments which the lowering of the surface has opened up on top, transforming them into surface depre作者: Lyme-disease 時間: 2025-3-24 11:15
https://doi.org/10.1007/978-3-8348-9288-1 opening up the possibility of examining the mineral composition of the clastic sediment layers found in them. In dolines, red and yellow sediments prevailed, occurring in several shades and transitioning from red to yellow and then to brown. All samples were similar in terms of their mineral compos作者: affluent 時間: 2025-3-24 17:23
https://doi.org/10.1007/978-3-8348-9288-1 cross-section of the cave was app. 6 m high, with a few metres of ceiling above it. In view of the knowledge available back then, it could be assumed that applying the palaeomagnetic method was the only way to undertake the dating of these sediments. The passage exhibited yellow layers of fluvial c作者: 連鎖 時間: 2025-3-24 21:04
https://doi.org/10.1007/978-3-8348-9288-1per main road, in the cutting which was formed during the construction of the Diva?a–Klanec motorway. The sampled profile consists of more than 5 m of alluvium in two main sequences. The lower sequence comprised ochre-coloured sandy to clayey sediments that were app. 3 m thick. These sediments were 作者: Verify 時間: 2025-3-25 00:06
https://doi.org/10.1007/978-3-8348-9288-1 and 50 m deep. The eastern part descends evenly and reaches its lowest accessible point at the altitude of 315 m, i.e. 47 m under the bottom of the tunnel. The western part ascends gently so that the final point lies at the altitude of 356 m, 6 m under the tunnel’s bottom. In addition to flowstone,作者: BOOM 時間: 2025-3-25 04:58
https://doi.org/10.1007/978-3-8348-9288-1cation over several karst periods and were subject to a number of karstification and epikarst development phases. Due to denudation, the epikarst, where the rock is markedly dissected by typical surface karst features, moves down the transverse profile of the karst system, through the traces of form作者: BUCK 時間: 2025-3-25 08:42
Nichtlineare Optik II: Vierwellenmischung,ured to the level of tectonic breccia. This is understandable, as the area in question is part of the Sava compressive wedge which has undergone several phases of tectonic processes. Unlike southwestern Slovenia, where Cretaceous limestone prevails, this karst developed in the Triassic and Jurassic 作者: 違抗 時間: 2025-3-25 13:58 作者: alliance 時間: 2025-3-25 17:35 作者: Laconic 時間: 2025-3-25 21:56
978-3-319-36732-3Springer International Publishing Switzerland 2016作者: 彎曲道理 時間: 2025-3-26 00:33
Introduction, Basin, and the Pannonian Basin with the Alps. Slovenian motorways entail an approx. 615 km long network of roads. Almost half of Slovenia consists of karst and more than half of the country’s water supply comes from karst aquifers. Slovenia is the country of the original Karst, which gave its name 作者: TERRA 時間: 2025-3-26 06:53 作者: FEIGN 時間: 2025-3-26 11:50 作者: Injunction 時間: 2025-3-26 14:17 作者: capsule 時間: 2025-3-26 18:37 作者: 食物 時間: 2025-3-26 23:55 作者: Vertical 時間: 2025-3-27 02:58
Unroofed Caves Provide Important Clues to the Karst Developmentd flowstone. It became clear during the motorway construction undertaking in Slovenia that unroofed caves constitute a relatively common karst landform. In fact, more common than karstologists had imagined before the karst surface was uncovered through earthworks. The various types of notches occurr作者: Commonwealth 時間: 2025-3-27 06:50
The Large Unroofed Cave Near Povired near the village of Povir. It contained flowstone, stalactites, stalagmites and various sediments. Inside the cave, flowstone has been preserved in the form of crusts, massive flowstone heaps, and free-standing stalagmites, but some broken off stalactites were also found. It is possible to recons作者: 表狀態(tài) 時間: 2025-3-27 11:46 作者: 體貼 時間: 2025-3-27 16:48
Composition of Sediments in Dolines opening up the possibility of examining the mineral composition of the clastic sediment layers found in them. In dolines, red and yellow sediments prevailed, occurring in several shades and transitioning from red to yellow and then to brown. All samples were similar in terms of their mineral compos作者: musicologist 時間: 2025-3-27 21:27 作者: ANTE 時間: 2025-3-27 22:58
Palaeomagnetic Research of an Unroofed Cave Near Kozinaper main road, in the cutting which was formed during the construction of the Diva?a–Klanec motorway. The sampled profile consists of more than 5 m of alluvium in two main sequences. The lower sequence comprised ochre-coloured sandy to clayey sediments that were app. 3 m thick. These sediments were 作者: maudtin 時間: 2025-3-28 03:20
Sediments in the S-647 Cave in the Kastelec Tunnel and 50 m deep. The eastern part descends evenly and reaches its lowest accessible point at the altitude of 315 m, i.e. 47 m under the bottom of the tunnel. The western part ascends gently so that the final point lies at the altitude of 356 m, 6 m under the tunnel’s bottom. In addition to flowstone,作者: Agronomy 時間: 2025-3-28 09:33
The History of Karstification on the Upper Cretaceous and Lower Paleogene Limestones in the Wider Kocation over several karst periods and were subject to a number of karstification and epikarst development phases. Due to denudation, the epikarst, where the rock is markedly dissected by typical surface karst features, moves down the transverse profile of the karst system, through the traces of form作者: Panacea 時間: 2025-3-28 10:52 作者: Mhc-Molecule 時間: 2025-3-28 14:40 作者: cardiovascular 時間: 2025-3-28 19:13 作者: sebaceous-gland 時間: 2025-3-28 23:01 作者: Biguanides 時間: 2025-3-29 03:20
https://doi.org/10.1007/978-3-8348-9213-3rstified. Due to the construction of the tunnel and extensive roadcuts, the impact of the activities affecting the Karst Edge and its hinterland was significant, in several places leading to the unearthing of today’s epikarst and a part of the vadose zone, both of which are also intersected with old作者: NIB 時間: 2025-3-29 10:43
https://doi.org/10.1007/978-3-8348-9213-3o dramatically, there are old caves and shafts opening up all the time in the course of the construction of the motorways. Old caves are either void or filled with alluvium. The caves were formed as a part of a system of cavities in a period when impermeable rocks had enclosed the aquifer higher up,作者: 意見一致 時間: 2025-3-29 12:24
https://doi.org/10.1007/978-3-8348-9213-3the development of the aquifer. Seeing as today the underground water level is 200?m and more below the surface, the traces of ancient water flow through the aquifer are now preserved only in caves and their respective alluvium. There was no indication of surface water flows that could have reshaped作者: Consensus 時間: 2025-3-29 16:07
https://doi.org/10.1007/978-3-8348-9213-3s the result of the high permeability of this part of the aquifer. The size of the passages suggests that they were passed by larger water flows which had originally completely filled the passages. It is assumed that a remnant of a flysch nappe was somewhere in the vicinity, feeding the aquifer with作者: 逢迎白雪 時間: 2025-3-29 23:46 作者: Bother 時間: 2025-3-30 00:55 作者: insurgent 時間: 2025-3-30 04:53
https://doi.org/10.1007/978-3-8348-9288-1rs were not far off. There were no relevant barriers for the water flow on its course from the ponors to the cave. The formation of stalactites/stalagmites and flowstone heaps does not reflect external influences, although the growth of the stalactites and stalagmites was interrupted several times b作者: Shuttle 時間: 2025-3-30 11:10 作者: 無王時期, 時間: 2025-3-30 13:29
https://doi.org/10.1007/978-3-8348-9288-1thite, lepidocrocite, hematite and maghemite, while the iron sulphide, pyrite, is also frequent. The colour of the weathered flysch is yellow to yellow-brown, while the surface and fissures, where the deposited sediments came into lengthier contact with atmospheric conditions, feature a typical tran作者: Self-Help-Group 時間: 2025-3-30 18:20
https://doi.org/10.1007/978-3-8348-9288-1 due to their drying or shifting on account of subsidence or tectonics. Certain parts of the profile were also heavily cemented with calcite, namely in the form of randomly positioned irregular bodies. In terms of their mineral composition, the sediments found in the cave are weathered remains of th作者: heartburn 時間: 2025-3-30 22:48
https://doi.org/10.1007/978-3-8348-9288-1he ochre-coloured intercalations in the upper part of the upper sequence may indicate the presence of eroded sediment comparable with the lower sequence. The thinning of cave ceilings through erosion and karst denudation triggered collapsing. The sediment originates most probably from the weathered 作者: Flawless 時間: 2025-3-31 02:24
https://doi.org/10.1007/978-3-8348-9288-1 cave is interesting because it is located deep under the surface and has been inaccessible until the tunnel began being constructed. What is more, this is not a sink cave in terms of origin, but it contains a lot of alluvium as well as vast quantities of collapsed stalagmites and stalactites. The b作者: 污點 時間: 2025-3-31 06:06 作者: 低三下四之人 時間: 2025-3-31 13:07
Nichtlineare Optik II: Vierwellenmischung,rst time. The old caves, through which streams were once flowing, attest to the lowering of the groundwater level, which reaches the surface only in the lowest-lying lowlands. A good part of the caves is filled with fine-grained sediment and has been transformed underneath it. The shaping of fissure作者: 辮子帶來幫助 時間: 2025-3-31 14:48 作者: 微塵 時間: 2025-3-31 19:27 作者: noxious 時間: 2025-4-1 00:11 作者: archaeology 時間: 2025-4-1 05:07
Unroofed Caves Near Kozina and Their Identificationo dramatically, there are old caves and shafts opening up all the time in the course of the construction of the motorways. Old caves are either void or filled with alluvium. The caves were formed as a part of a system of cavities in a period when impermeable rocks had enclosed the aquifer higher up,作者: 有角 時間: 2025-4-1 07:01 作者: enchant 時間: 2025-4-1 14:07 作者: 瑣碎 時間: 2025-4-1 17:45 作者: gregarious 時間: 2025-4-1 22:12
Unroofed Caves Provide Important Clues to the Karst Developmented caves filled with all types of alluvium were discovered. There were several attempts at typification of the characteristic shapes of unroofed caves and to design partial models to explain their typical formation processes. The surface and subcutaneous dissolution of carbonate rock and its disinte作者: Salivary-Gland 時間: 2025-4-2 00:26 作者: 前奏曲 時間: 2025-4-2 04:30
Origin and Mineral Composition of Clastic Sediments on the Karst Surface Around Diva?a no longer protected against weathering. Denuded cave sediments represent an important source of soil in the Karst. Sediments and cave passages of the Brezstropa jama unroofed cave enable us to partially depict the time in which these caves were formed. It can be assumed that the cave was completely
