標題: Titlebook: Campi Flegrei; A Restless Caldera i Giovanni Orsi,Massimo D‘Antonio,Lucia Civetta Book 2022 Springer-Verlag GmbH Germany, part of Springer [打印本頁] 作者: 選民 時間: 2025-3-21 19:57
書目名稱Campi Flegrei影響因子(影響力)
書目名稱Campi Flegrei影響因子(影響力)學(xué)科排名
書目名稱Campi Flegrei網(wǎng)絡(luò)公開度
書目名稱Campi Flegrei網(wǎng)絡(luò)公開度學(xué)科排名
書目名稱Campi Flegrei被引頻次
書目名稱Campi Flegrei被引頻次學(xué)科排名
書目名稱Campi Flegrei年度引用
書目名稱Campi Flegrei年度引用學(xué)科排名
書目名稱Campi Flegrei讀者反饋
書目名稱Campi Flegrei讀者反饋學(xué)科排名
作者: 蕁麻 時間: 2025-3-21 20:19 作者: rectum 時間: 2025-3-22 02:39 作者: 名字的誤用 時間: 2025-3-22 06:18 作者: hangdog 時間: 2025-3-22 11:10 作者: Genetics 時間: 2025-3-22 14:28
Rheological Properties of the Magmas Feeding the Campi Flegrei Caldera (Italy) and Their Influence rei caldera volcanism. Viscosity and density control flow and diffusion, and?thus multicomponent?convection and chemical mobility in the magma chamber. These, in turn, are thought to constrain magma mixing processes in the system. Our main goal is to summarise and analyse mixing experiments using na作者: Genetics 時間: 2025-3-22 20:32
Magma Chamber Dynamics at the Campi Flegrei Caldera, Italy, have been largely driven by magma chamber processes like fractional crystallisation, magma mixing, and volatile degassing. These processes have been intensely investigated with a variety of approaches that are described in many chapters of this book, and more specifically, in Chaps. .; .. In this c作者: Desert 時間: 2025-3-22 23:49
The Permanent Monitoring System of the Campi Flegrei Caldera, Italy,n the Campi Flegrei caldera. Eruptive history of this active volcano shows that the majority of the eruptive events has been characterised by high explosivity and was accompanied by pyroclastic density currents. Its last eruption occurred in AD 1538 and in the next centuries the Campi Flegrei calder作者: 裂口 時間: 2025-3-23 04:56
The Hydrothermal System of the Campi Flegrei Caldera, Italy,The Campi Flegrei caldera has been undergoing unrest since 1950, as evidenced by recurrent bradyseismic episodes accompanied by manifest changes in the degassing budget, degassing patterns and in the composition of the fumarolic fluids. In-depth analysis of geochemical and geophysical datasets acqui作者: 懸掛 時間: 2025-3-23 09:17 作者: 廣大 時間: 2025-3-23 12:49
Source Modelling from Ground Deformation and Gravity Changes at the Campi Flegrei Caldera, Italy,?m cumulative uplift, occurring at a rate of ~1?m/yr. Both events were accompanied by seismic activity, gravity changes and compositional variations of volcanic gases but no eruption took place. During the following decades, the area has been slowly subsiding but minor uplift episodes (~a few cm), s作者: 能量守恒 時間: 2025-3-23 16:28 作者: cathartic 時間: 2025-3-23 21:15 作者: LUCY 時間: 2025-3-24 01:38 作者: pulmonary 時間: 2025-3-24 06:23
The Urban Development of Campi Flegrei, Italy,mercially and?strategically advantageous position in the Mediterranean basin. After a period of frequent eruptions that affected the environment and forced indigenous farmers temporarily to abandon the area after each event, in 740 BC Campi Flegrei were chosen by Chalcidian Greeks from Ischia to est作者: STRIA 時間: 2025-3-24 08:55 作者: 萬神殿 時間: 2025-3-24 12:56
,Methoden für instation?re Str?mungen,m) partially molten bodies. Seismic attenuation tomography provides information complementary to velocity tomography, defining lateral lithological changes and the geometry of onshore and offshore fluid and magma bodies down to 4?km depth. Once compared with seismic analyses, gravity data highlight 作者: 捕鯨魚叉 時間: 2025-3-24 16:18
https://doi.org/10.1007/978-3-540-68228-8ted, eventually feeding the volcanic activity. These magmatic components originated through a complex interplay of magma supply from a variably-enriched mantle source, and crustal contamination processes occurring at depth. Mingling/mixing among these isotopically-distinct magmatic components, as we作者: 透明 時間: 2025-3-24 20:33 作者: 用不完 時間: 2025-3-25 01:06
,L?sung linearer Gleichungssysteme,ion of Concentration Variance or Concentration Variance Decay. This enables the measurement of mobility for all elements present in the melt simultaneously. Comparing experimental and natural data clearly?confirm the?unavoidability of mixing during the replenishment history of the caldera reservoir(作者: peak-flow 時間: 2025-3-25 03:49
,Methoden für instation?re Str?mungen,at Campi Flegrei caldera are accounted for. They include the more chemically evolved, partially degassed nature of magmas emplaced at shallow depths, and the likely occurrence of multiple reservoirs with different depth, size and shape which can be connected at certain stages during system evolution作者: 積習(xí)已深 時間: 2025-3-25 09:02
https://doi.org/10.1007/978-3-642-79353-0ent multi-parametric monitoring system. All the recorded h24 continuous data are transmitted to the Monitoring Room of the Osservatorio Vesuviano in Naples, where they are acquired, processed and evaluated to define changes in the dynamical state of the volcano. The caldera, since the end of 2004, i作者: 嚙齒動物 時間: 2025-3-25 13:33
Herbert Oertel Jr.,Eckart Lauriene in axis with the Solfatara fumaroles, which represents a relatively high permeability zone allowing hot fluid ascent from depth to the shallower portions of the hydrothermal system. Pulsed injections of hot magmatic fluids (CO.-rich and CH.-poor oxidised fluids) at the bottom of the hydrothermal s作者: 免費 時間: 2025-3-25 19:17 作者: 廚房里面 時間: 2025-3-25 20:03
Geometrie- und Netzgenerierung, techniques. Deformation and gravity data provide important constraints on depth, volume, mass density and dislocation mechanisms accompanying magma emplacement processes. The correct evaluation of these parameters is strongly conditioned by simplifying assumptions built in the different inversion p作者: 傾聽 時間: 2025-3-26 01:22 作者: 先兆 時間: 2025-3-26 08:20 作者: 嗎啡 時間: 2025-3-26 12:03 作者: 遠地點 時間: 2025-3-26 13:08
https://doi.org/10.1007/978-3-662-46544-8and the AD 1538 Monte Nuovo eruption did not discourage people from living in the area. Campi Flegrei have undergone socio-economic development which for most of its history has been sustainable. Only with industrialisation over recent decades, has it become unsustainable. This unsustainable develop作者: Cryptic 時間: 2025-3-26 18:15
Volcanic and Deformation History of the Campi Flegrei Volcanic Field, Italy,nce during which two widespread paleosols formed. During each epoch, the eruptions occurred at mean time intervals of tens of years. The last event produced the Monte Nuovo tuff cone in AD 1538, after?~3,000?years of quiescence. Deformation mostly consists of a resurgence process that has generated 作者: 雜役 時間: 2025-3-26 21:20 作者: BROW 時間: 2025-3-27 04:07 作者: 不可磨滅 時間: 2025-3-27 07:51 作者: 旁觀者 時間: 2025-3-27 13:30 作者: 嘮叨 時間: 2025-3-27 13:47 作者: photopsia 時間: 2025-3-27 20:00
The Permanent Monitoring System of the Campi Flegrei Caldera, Italy,ent multi-parametric monitoring system. All the recorded h24 continuous data are transmitted to the Monitoring Room of the Osservatorio Vesuviano in Naples, where they are acquired, processed and evaluated to define changes in the dynamical state of the volcano. The caldera, since the end of 2004, i作者: analogous 時間: 2025-3-28 01:23 作者: white-matter 時間: 2025-3-28 04:16 作者: 放大 時間: 2025-3-28 08:36
Source Modelling from Ground Deformation and Gravity Changes at the Campi Flegrei Caldera, Italy, techniques. Deformation and gravity data provide important constraints on depth, volume, mass density and dislocation mechanisms accompanying magma emplacement processes. The correct evaluation of these parameters is strongly conditioned by simplifying assumptions built in the different inversion p作者: CESS 時間: 2025-3-28 13:05
Volcanic Hazard Assessment at the Campi Flegrei Caldera, Italy,nd a non-negligible vent opening probability spreads over the whole caldera. The inter-event times of volcanic eruptions span from a few years to thousands of years. Within the epochs of activity, the mean recurrence time is tens of years, and intra-epoch temporal groups are evident. The probability作者: omnibus 時間: 2025-3-28 16:35
Landslide Hazard and Risk in the Campi Flegrei Caldera, Italy,isation of the area, such a hazard results in a quite high risk. In recent years, a number of structural countermeasures, including low-impact soil bioengineering techniques, have been introduced as to mitigate the landslide risk in the Neapolitan-Phlegraean area. However, a paradigm shift is strong作者: 的’ 時間: 2025-3-28 19:31
Building Stones and Technological Materials of the Campi Flegrei Caldera, Italy,building portals, columns) further corroborates the aforementioned. When the Phlegraean rocks were used for purely structural functions, they were covered with plaster made with Phlegraean sands and aggregates, or, less frequently, with stone slabs from other exploitation sites in the Campania regio作者: HAIRY 時間: 2025-3-29 00:35 作者: alcohol-abuse 時間: 2025-3-29 05:17 作者: Anticoagulant 時間: 2025-3-29 07:23 作者: conjunctiva 時間: 2025-3-29 14:57
,L?sung linearer Gleichungssysteme, studies, experimental petrology and phase equilibria modelling from the existing literature are also presented and critically evaluated. On such basis, a model for the Campi Flegrei magmatic system is proposed, in an attempt to construct a reference framework from which reasonable speculations of its possible future behaviour could be obtained.作者: ENDOW 時間: 2025-3-29 19:03 作者: OCTO 時間: 2025-3-29 20:34 作者: 無可非議 時間: 2025-3-30 03:00
Book 2022graph synthesises the current knowledge of this volcano, through different review chapters. Each chapter of this book is dedicated to a specific volcanological aspect, authored by well-recognised experts. The volume attempts to cross the barriers between the volcanological, geological, geochemical a作者: 和平主義 時間: 2025-3-30 06:46 作者: 符合國情 時間: 2025-3-30 12:02
Springer-Verlag GmbH Germany, part of Springer Nature 2022作者: 最高峰 時間: 2025-3-30 14:00 作者: 鋼盔 時間: 2025-3-30 17:23
,Methoden für instation?re Str?mungen,d the structure of the crust beneath the Campi Flegrei caldera. We describe the main lithological and structural discontinuities defined through these observations, illustrate their geophysical responses, and discuss the constraints they give to the understanding of magmatic and volcanic processes. 作者: V洗浴 時間: 2025-3-30 20:55