標(biāo)題: Titlebook: Geothermics and Geothermal Energy; Ladislaus Rybach,Lajos Stegena Book 1979 Springer Basel AG 1979 earth science.energy.engineering.geolog [打印本頁] 作者: Exacting 時(shí)間: 2025-3-21 18:48
書目名稱Geothermics and Geothermal Energy影響因子(影響力)
書目名稱Geothermics and Geothermal Energy影響因子(影響力)學(xué)科排名
書目名稱Geothermics and Geothermal Energy網(wǎng)絡(luò)公開度
書目名稱Geothermics and Geothermal Energy網(wǎng)絡(luò)公開度學(xué)科排名
書目名稱Geothermics and Geothermal Energy被引頻次
書目名稱Geothermics and Geothermal Energy被引頻次學(xué)科排名
書目名稱Geothermics and Geothermal Energy年度引用
書目名稱Geothermics and Geothermal Energy年度引用學(xué)科排名
書目名稱Geothermics and Geothermal Energy讀者反饋
書目名稱Geothermics and Geothermal Energy讀者反饋學(xué)科排名
作者: CHIDE 時(shí)間: 2025-3-21 21:59
Joshua Lipton,Zenon Tederko,Eric Englishhermal research that includes (1) study of geothermal processes on crustal and local scales, (2) regional evaluations, (3) intensive study of type systems before and during exploitation, (4) improvement of exploration techniques, and (5) investigation of geoenvironmental constraints.作者: 他很靈活 時(shí)間: 2025-3-22 01:36 作者: DEMN 時(shí)間: 2025-3-22 07:39
Variation of Continental Mantle Heat Flow with Age: Possibility of Discriminating Between Thermal Mo= 500 (1/ .) for the variation of oceanic heat flow . (in mW/M.) with age . (in million years) provides a reasonably good fit to the mantle heat flow data. The constant thickness plate model however, is found to be unsatisfactory in explaining the variation of continental mantle heat flow with age.作者: 束縛 時(shí)間: 2025-3-22 08:51 作者: STALE 時(shí)間: 2025-3-22 16:10 作者: STALE 時(shí)間: 2025-3-22 18:13
Equity in the Civil Law Traditionone between crustal thickness and heat flow. A general conclusion could be drawn that the heat flow distribution over the Romanian territory seems to be governed by processes taking place in the upper mantle, rather than by the radioactive decay within the crust.作者: 花束 時(shí)間: 2025-3-22 23:23 作者: 持久 時(shí)間: 2025-3-23 02:43
The Relationship Between Seismic Velocity and Radioactive Heat Production in Crustal Rocks: An Exponec which follows the exponential law: ... = . exp (- ..., where the numerical factors . and . depend on . pressure. A graph is given by means of which the heat production distribution . can be obtained for any given ... structure.作者: 顯而易見 時(shí)間: 2025-3-23 06:00
Risk Management of Vanilla Equity Options,ortion of crustal thinning, and requires a magma source at 75 km depth with differentiation at 11 km depth. The model is applied in outline to the development of continental and orogenic volcanism in New Zealand.作者: 磨碎 時(shí)間: 2025-3-23 11:45
Venture Capital and Contracting,lley, Coso Hot Springs, and the Danville region, all in California. The first two of these areas are known for their Holocene volcanism and geothermal potential, which is consistent with crustal spreading and magmatic intrusion. The third example, however, shows no evidence for volcanism or geothermal activity at the surface.作者: helper-T-cells 時(shí)間: 2025-3-23 14:55
Jelena Radi?i?,Andreas Pettersenhe hypothesis that the Apennine chain is intersected by two arcuate structures: the first from Liguria to Latium is very probably a continental arc, that is an arc which occurs within a continent, and the second from Campania to Calabria is very similar from geophysical evidence to the classic island arcs.作者: DOLT 時(shí)間: 2025-3-23 20:04
The Latch Correspondence Problemtly with no consistent trend. To the east, on the coast of Israel, the heat flow values increase, ranging from 36.6 ± 22.4 to 56.7 ± 14.2 mW/m. along a SSE trend. The trend apparently correlates with an increase in crustal thickness, which is about 23 km at the north-west base of the Nile-Delta-cone, and close to 40 km beneath Israel.作者: consent 時(shí)間: 2025-3-24 02:06 作者: 鞭打 時(shí)間: 2025-3-24 06:24
Earthquake Swarms and Local Crustal Spreading Along Major Strike-slip Faults in Californialley, Coso Hot Springs, and the Danville region, all in California. The first two of these areas are known for their Holocene volcanism and geothermal potential, which is consistent with crustal spreading and magmatic intrusion. The third example, however, shows no evidence for volcanism or geothermal activity at the surface.作者: 產(chǎn)生 時(shí)間: 2025-3-24 07:36 作者: barium-study 時(shí)間: 2025-3-24 10:57
Review of Heat Flow Data from the Eastern Mediterranean Regiontly with no consistent trend. To the east, on the coast of Israel, the heat flow values increase, ranging from 36.6 ± 22.4 to 56.7 ± 14.2 mW/m. along a SSE trend. The trend apparently correlates with an increase in crustal thickness, which is about 23 km at the north-west base of the Nile-Delta-cone, and close to 40 km beneath Israel.作者: 走調(diào) 時(shí)間: 2025-3-24 17:04
An Exchange and Its Value Chainec which follows the exponential law: ... = . exp (- ..., where the numerical factors . and . depend on . pressure. A graph is given by means of which the heat production distribution . can be obtained for any given ... structure.作者: arbovirus 時(shí)間: 2025-3-24 19:03
https://doi.org/10.1007/978-3-0348-6525-8earth science; energy; engineering; geology; geophysics; geothermal energy; physics; renewable energy作者: 馬籠頭 時(shí)間: 2025-3-24 23:13
https://doi.org/10.1007/978-3-658-31266-4atic equilibrium and in which fractional crystallization of the magma or partial melting of the ambient rock can occur. The density structure of the crust has a powerful effect in trapping magma and thereby in controlling the occurrence of high level geothermal systems. The model is tested in Part I作者: Capitulate 時(shí)間: 2025-3-25 03:38
Risk Management of Vanilla Equity Options,ertiary sedimentary and volcanic region of central West Greenland : the thickness of sedimentary rock; the thickness of the pillow breccias ; the total thickness of the lava pile; the depth of the post volcanic paleosurface. The local development is largely determined by a single parameter, the prop作者: Countermand 時(shí)間: 2025-3-25 10:17
https://doi.org/10.1057/9781137335548rature and thickness from conduction-model estimates depends upon the mechanical mode of extension and upon how rapidly extension is (and has been) taking place. Present knowledge of these processes is insufficient to provide adequate constraints on thermal models. The high and variable regional hea作者: 顧客 時(shí)間: 2025-3-25 14:09
Venture Capital and Contracting, between earthquake swarms and local crustal spreading. Local crustal spreading is required by the geometry of dextral offsets when, as in the San Andreas system, faults have dominantly strike-slip motion with right-lateral displacement. Three clear examples of this relation occur in the Imperial Va作者: Flustered 時(shí)間: 2025-3-25 16:43 作者: Latency 時(shí)間: 2025-3-25 23:38 作者: 沉默 時(shí)間: 2025-3-26 02:19 作者: STERN 時(shí)間: 2025-3-26 06:32
Equity Issues in Teacher Assessment temperatures, gradients and local heat flow patterns. In areas without data the heat flow field was extrapolated on the basis of the regional tectonic structure and the observed correlation of heat flow and the age of the last tectono-thermal event. The heat flow pattern as obtained in the map may 作者: Pillory 時(shí)間: 2025-3-26 10:17 作者: 存心 時(shí)間: 2025-3-26 13:13 作者: 考得 時(shí)間: 2025-3-26 17:14 作者: 脆弱帶來 時(shí)間: 2025-3-26 23:28 作者: chemoprevention 時(shí)間: 2025-3-27 02:41
The Latch Correspondence Problem east of Crete (Levantine Sea), Cyprus, and northern Egypt. The average of the marine heat flow measurements in the Levantine Sea is 25.7 ± 8.4 mW/m., and the heat flow on Cyprus is 28.0 ±8.0 mW/m.. The estimated values of heat flow in northern Egypt range from 38.3 ± 7.0 to 49.9 ±9.3 mW/m., apparen作者: 繁殖 時(shí)間: 2025-3-27 06:43 作者: 衰弱的心 時(shí)間: 2025-3-27 13:09
Appendix B: The Robin Hood Model,, and high to the east (80–90 mW m.). The average heat flow in CPC and the low heat generation (less than 1 μW m.) indicate that a relatively large amount of heat flows upwards into the crust which is generally quite cool. Until two million years ago the Explorer plate underthrust this part of the A作者: 未完成 時(shí)間: 2025-3-27 17:23
https://doi.org/10.1007/978-981-16-7073-2latively low temperature gradients in the range 6 to 20°C/km while younger sedimentary basins are characterized by gradients in the range 15 to 35°C/km. An inverse correlation between geothermal gradient and tectonic age has been observed. This as well as the favourable hydrological conditions sugge作者: badinage 時(shí)間: 2025-3-27 18:08
Vinylchlorid als karzinogene Substanz,th warm aquifers. The most promising reservoirs have been found in highly permeable Upper Triassic sand and sandstone beds, which cover at least 5000 km. at depths of 2000–3000 m and at temperatures of 60–100°C. The porosity of the main reservoir is of 15–25%, and the permeability is presumed to be 作者: alcohol-abuse 時(shí)間: 2025-3-27 21:59 作者: prostatitis 時(shí)間: 2025-3-28 02:26 作者: 高興一回 時(shí)間: 2025-3-28 09:53
Culturally Responsive Culture of Assessment5–40 mW/m.). Increased heat flow (>50 mW/m.) has been found in the Dniepr-Donetz depression. The area south of the East European Platform is characterized by highly variable heat flow (55–100 mW/m.). Some geophysical implications are discussed.作者: 地名詞典 時(shí)間: 2025-3-28 12:48 作者: companion 時(shí)間: 2025-3-28 15:34
Heat Flow Map of the European Part of the U.S.S.R.5–40 mW/m.). Increased heat flow (>50 mW/m.) has been found in the Dniepr-Donetz depression. The area south of the East European Platform is characterized by highly variable heat flow (55–100 mW/m.). Some geophysical implications are discussed.作者: 枕墊 時(shí)間: 2025-3-28 18:49
978-3-0348-6527-2Springer Basel AG 1979作者: harpsichord 時(shí)間: 2025-3-28 23:08 作者: Detoxification 時(shí)間: 2025-3-29 04:06
https://doi.org/10.1007/978-3-663-02416-3Preliminary investigations of the geothermal energy potential in Sweden are being carried out in crystalline rocks of Precambrian age, as well as in the Triassic Buntsandstone. The geothermal potential of fracture zones is also being investigated. Different methods for prospecting have been tried and compared.作者: PLE 時(shí)間: 2025-3-29 09:45 作者: rods366 時(shí)間: 2025-3-29 15:01
Magma Traps: Part I, Theoryatic equilibrium and in which fractional crystallization of the magma or partial melting of the ambient rock can occur. The density structure of the crust has a powerful effect in trapping magma and thereby in controlling the occurrence of high level geothermal systems. The model is tested in Part I作者: DENT 時(shí)間: 2025-3-29 18:16 作者: Gullible 時(shí)間: 2025-3-29 21:26 作者: 放肆的你 時(shí)間: 2025-3-30 00:08
Earthquake Swarms and Local Crustal Spreading Along Major Strike-slip Faults in California between earthquake swarms and local crustal spreading. Local crustal spreading is required by the geometry of dextral offsets when, as in the San Andreas system, faults have dominantly strike-slip motion with right-lateral displacement. Three clear examples of this relation occur in the Imperial Va作者: conflate 時(shí)間: 2025-3-30 05:23 作者: archaeology 時(shí)間: 2025-3-30 08:28 作者: Infusion 時(shí)間: 2025-3-30 16:27
The Degree of Metamorphism of Organic Matter in Sedimentary Rocks as a Paleo-Geothermometer, Appliedganic matter increases continually. Apart from temperature, the slowly reacting chemical compounds of the organic matter strongly depend on time, too..It is shown that the coal rank is proportional to the integral of temperature and time of burial (.) for the Tertiary sedimentary rocks of the Upper 作者: Aqueous-Humor 時(shí)間: 2025-3-30 17:37
The Preliminary Heat Flow Map of Europe and Some of its Tectonic and Geophysical Implications temperatures, gradients and local heat flow patterns. In areas without data the heat flow field was extrapolated on the basis of the regional tectonic structure and the observed correlation of heat flow and the age of the last tectono-thermal event. The heat flow pattern as obtained in the map may 作者: Meager 時(shí)間: 2025-3-31 00:12 作者: alabaster 時(shí)間: 2025-3-31 00:58
Mantle Heat Flow and Geotherms for Major Tectonic Units in Central Europeeneration models for the crust in the Paleozoic Platform region, the Sudetic Mountains (Variscan Internides) and the European Precambrian Platform show considerable differences in mantle heat flow and temperatures. At the base of the crust variations from 440–510°C in the models of Precambrian Platf作者: 凹槽 時(shí)間: 2025-3-31 08:34
On the Geothermal Regime of Some Tectonic Units in Romania0–120 mW m. for the Neogene volcanic area. Temperature-depth profile and some geophysical implications of the low values for the Transylvanian Depression are discussed, rendering evident clear-cut differences between this tectonic unit and other Neogene depressions. The heat flow values for the othe作者: 宮殿般 時(shí)間: 2025-3-31 10:14
Heat Flow in Italygeological features with the following results: foreland areas, 55+19 mW m., foredeep areas, 45 ± 21 mW m .; folded regions and intermountain depressions, 76 ± 29 mW m.. In volcanic areas the heat flow rises to in excess of 600 mW m.. From a tectonic point of view, these values are consistent with t作者: choleretic 時(shí)間: 2025-3-31 15:15 作者: 啟發(fā) 時(shí)間: 2025-3-31 20:19
Geothermal Resource Assessment of the United Statest some reasonable future time. In the United States, the Geological Survey is responsible for preparing geothermal assessments based on the best available data and interpretations. Updates are required every few years owing to increasing knowledge, enlarging data base, improving technology, and chan作者: emission 時(shí)間: 2025-3-31 23:19 作者: BUMP 時(shí)間: 2025-4-1 03:00 作者: 連系 時(shí)間: 2025-4-1 08:52
