標(biāo)題: Titlebook: Geological Evolution of the Mediterranean Basin; Raimondo Selli Comme Daniel Jean Stanley,Forese-Carlo Wezel Book 1985 Springer-Verlag New [打印本頁(yè)] 作者: culinary 時(shí)間: 2025-3-21 19:46
書目名稱Geological Evolution of the Mediterranean Basin影響因子(影響力)
書目名稱Geological Evolution of the Mediterranean Basin影響因子(影響力)學(xué)科排名
書目名稱Geological Evolution of the Mediterranean Basin網(wǎng)絡(luò)公開度
書目名稱Geological Evolution of the Mediterranean Basin網(wǎng)絡(luò)公開度學(xué)科排名
書目名稱Geological Evolution of the Mediterranean Basin被引頻次
書目名稱Geological Evolution of the Mediterranean Basin被引頻次學(xué)科排名
書目名稱Geological Evolution of the Mediterranean Basin年度引用
書目名稱Geological Evolution of the Mediterranean Basin年度引用學(xué)科排名
書目名稱Geological Evolution of the Mediterranean Basin讀者反饋
書目名稱Geological Evolution of the Mediterranean Basin讀者反饋學(xué)科排名
作者: 夾克怕包裹 時(shí)間: 2025-3-21 23:02
Geological Information from Satellite Surveys of the Mediterranean Regioned on satellite images illustrate the existence of all classes of brittle fractures in the upper crust. Lineament patterns suggest the tectonic patterns for a given region, but it is necessary to “field check” any area for which lineament maps are prepared. It is critical that such studies be carrie作者: 辯論 時(shí)間: 2025-3-22 04:15
Seismicity of the Mediterranean Basinbetween the African and Eurasian plates. This boundary is of a complex nature, and its dynamics are the consequence of the opening of the Atlantic Ocean and the closing of the Mediterranean Sea. Main tectonic features are of compressive character, with only very localized zones undergoing horizontal作者: 機(jī)制 時(shí)間: 2025-3-22 06:33 作者: 滑動(dòng) 時(shí)間: 2025-3-22 10:03
Some Boundary Conditions for the Evolution of the Mediterranean RegionGondwanaland. The relative motions of stable Africa relative to stable Europe, and vice versa, have been calculated from recently available data. The motions have been shown as increments and as total displacements. The total displacements have also been calculated for the hotspots frame both for st作者: Cpr951 時(shí)間: 2025-3-22 13:30 作者: Cpr951 時(shí)間: 2025-3-22 20:20
Tectonic Evolution of the Tyrrhenian Searoplates from the Upper Cretaceous to the middle Pliocene. During this time span the Tyrrhenian Alps and Apennines were formed. From the Tortonian until the present a process of oceanization by mantle diapirism took place in the Tyrrhenian area associated with an extensional tectonic regime oriented作者: 變形詞 時(shí)間: 2025-3-23 00:06
Structural Features and Basin Tectonics of the Tyrrhenian Sea Its bilateral symmetry, which gives it the character of an interarc basin, is also manifested by the deep crustal configuration that should indicate opposite-vergent arcuate overthrusting (obduction) of the Tyrrhenian oceanic crust onto the Alpine (modern inactive front) and the Apennine (active fr作者: 公共汽車 時(shí)間: 2025-3-23 02:13
Recent Geological Evolution of the Adriatic Seae correlated with those on land. For example, the Sabbie di Asti Formation extends offshore from the Po Valley into the Adriatic Basin to the region immediately east of Ancona. Southward, the equivalent unit is the Sabbie di Carassai Formation, composed of basinal turbidites. In the southwestern par作者: 舊石器時(shí)代 時(shí)間: 2025-3-23 07:50
Structure and Evolution of the Central Mediterranean (Pelagian and Ionian Seas)riassic, produced continental rifting with prominent effects in the Streppenosa Trough (Sicily-Malta platform area) and in the Ionian Sea. A second extensional phase occurred in the Middle Jurassic and opened the Ionian Sea and Eastern Mediterranean. The Pelagian Sea and Sirte Rise (excluding the up作者: 縮減了 時(shí)間: 2025-3-23 09:58
Geophysics and Geodynamic Implications for the Evolution of the Hellenidesappears that the continental crust has been stretched considerably and thinned to about half its original thickness. The direction of expansion is north-south and northwest-southeast. In contrast to the Aegean Sea where tensional tectonics prevail, the outer Hellenic zones are structurally in a phas作者: flavonoids 時(shí)間: 2025-3-23 17:03
Slice Tectonics in the Eastern Mediterranean Basinve played a major role in shaping the Eastern Mediterranean. The first one, the Pelusium system, composed of the Dead Sea, Pelusium Line, and Qattara-Eratosthenes shears, is primarily responsible for the structure of the eastern Levantine Basin and the Levant. The other one, composed of the Pliny-Si作者: DUCE 時(shí)間: 2025-3-23 19:54
Neogene and Quaternary Mediterranean Volcanism: The Tyrrhenian Examplerrhenian volcanic belt, i.e., from southern Tuscany to Latium and Campania on the Apennine coastal range, Aeolian Islands, Ustica, Etna, and Sardinia. Discrepancies exist as to the origin of these fluids. Most authors suggest that the metasomatizing fluids originate from dehydration of a subducted l作者: interlude 時(shí)間: 2025-3-23 22:21
Plio-Quaternary Sedimentation and Tectonics in the Ionian Area: Clues to the Recent Evolution of thecurred since the Neogene. This evolution supports the model of Messinian shallow-water evaporation within a shallow basin setting. Sedimentary facies indicate a direct relation between Messinian sedimentation and rate of basin subsidence, the latter calculated at about 1 m/1000 years. The general pa作者: MEAN 時(shí)間: 2025-3-24 03:00
Models of Upper Miocene Evaporite Genesis in the Mediterranean Regionevaporite basins, such as the barred basin with one-way flow, the deep-water, wind-driven up welling, sebkha, or broad saturation shelf models, appears to be applicable to these Mediterranean evaporite cycles nor, for that matter, a model of a desiccating deep basin. Taking into account several acce作者: GIDDY 時(shí)間: 2025-3-24 07:52 作者: habile 時(shí)間: 2025-3-24 14:21
Book 1985e biology, and ecology and man‘s influence on the natural Medi- terranean regime. At a conference held in Banyuls-sur-Mer, France, in August 1979, Profes- sor Raimondo Selli was urged by some panel members to initiate an Ad- vanced Research Institute (ARI) that would focus primarily on the geologi- 作者: 親屬 時(shí)間: 2025-3-24 17:58
phy, marine biology, and ecology and man‘s influence on the natural Medi- terranean regime. At a conference held in Banyuls-sur-Mer, France, in August 1979, Profes- sor Raimondo Selli was urged by some panel members to initiate an Ad- vanced Research Institute (ARI) that would focus primarily on the geologi- 978-1-4613-8574-5978-1-4613-8572-1作者: Estimable 時(shí)間: 2025-3-24 20:25
Aspects of the Late Cenozoic Evolution of the Aegean Region作者: capsaicin 時(shí)間: 2025-3-25 01:29
https://doi.org/10.1007/978-3-662-28948-8ill moderately rises and thins toward the west; excessive sediment accumulation has taken place in these troughs since Paleozoic or even late Precambrian time. The Levantine Basin, with its 15–16 km thick sedimentary sequence, is therefore considered a relict of the Tethys Ocean, which is of an appr作者: ASSET 時(shí)間: 2025-3-25 04:23 作者: GONG 時(shí)間: 2025-3-25 10:49
https://doi.org/10.1007/978-3-642-94365-2ed on satellite images illustrate the existence of all classes of brittle fractures in the upper crust. Lineament patterns suggest the tectonic patterns for a given region, but it is necessary to “field check” any area for which lineament maps are prepared. It is critical that such studies be carrie作者: 小蟲 時(shí)間: 2025-3-25 11:53 作者: 隱士 時(shí)間: 2025-3-25 18:08
https://doi.org/10.1007/978-3-662-41335-7mental data are few, but their meaning can be extended areally using gravity anomalies. Although constituting different geologic settings, all these basins are relatively young or rejuvenated; their collapse is revealed by strong vertical or subvertical faults systems, and subsidence is continuing. 作者: 碎石 時(shí)間: 2025-3-25 20:46
Herabsetzung der Schmerzempfindung,Gondwanaland. The relative motions of stable Africa relative to stable Europe, and vice versa, have been calculated from recently available data. The motions have been shown as increments and as total displacements. The total displacements have also been calculated for the hotspots frame both for st作者: angina-pectoris 時(shí)間: 2025-3-26 00:22 作者: Blasphemy 時(shí)間: 2025-3-26 06:26 作者: 潛伏期 時(shí)間: 2025-3-26 11:17
,Orientierung über die Elektronentheorie, Its bilateral symmetry, which gives it the character of an interarc basin, is also manifested by the deep crustal configuration that should indicate opposite-vergent arcuate overthrusting (obduction) of the Tyrrhenian oceanic crust onto the Alpine (modern inactive front) and the Apennine (active fr作者: LITHE 時(shí)間: 2025-3-26 14:58 作者: Introvert 時(shí)間: 2025-3-26 18:26
Die neueste Entwicklung der Wasserhaltung,riassic, produced continental rifting with prominent effects in the Streppenosa Trough (Sicily-Malta platform area) and in the Ionian Sea. A second extensional phase occurred in the Middle Jurassic and opened the Ionian Sea and Eastern Mediterranean. The Pelagian Sea and Sirte Rise (excluding the up作者: 相同 時(shí)間: 2025-3-26 21:41 作者: 合唱團(tuán) 時(shí)間: 2025-3-27 02:55
https://doi.org/10.1007/978-3-662-28948-8ve played a major role in shaping the Eastern Mediterranean. The first one, the Pelusium system, composed of the Dead Sea, Pelusium Line, and Qattara-Eratosthenes shears, is primarily responsible for the structure of the eastern Levantine Basin and the Levant. The other one, composed of the Pliny-Si作者: 驚呼 時(shí)間: 2025-3-27 07:18
https://doi.org/10.1007/978-3-0348-4168-9rrhenian volcanic belt, i.e., from southern Tuscany to Latium and Campania on the Apennine coastal range, Aeolian Islands, Ustica, Etna, and Sardinia. Discrepancies exist as to the origin of these fluids. Most authors suggest that the metasomatizing fluids originate from dehydration of a subducted l作者: 苦澀 時(shí)間: 2025-3-27 09:41
Erratum to: Die Tanninfarbstoffe,curred since the Neogene. This evolution supports the model of Messinian shallow-water evaporation within a shallow basin setting. Sedimentary facies indicate a direct relation between Messinian sedimentation and rate of basin subsidence, the latter calculated at about 1 m/1000 years. The general pa作者: 飛行員 時(shí)間: 2025-3-27 15:33 作者: 泄露 時(shí)間: 2025-3-27 20:16
https://doi.org/10.1007/978-1-4613-8572-1Evolution; Ocean; Oceanography; geophysics; marine; plankton作者: 按時(shí)間順序 時(shí)間: 2025-3-27 23:29 作者: 愛(ài)好 時(shí)間: 2025-3-28 03:00 作者: CLOWN 時(shí)間: 2025-3-28 06:15 作者: Gyrate 時(shí)間: 2025-3-28 12:35 作者: dissent 時(shí)間: 2025-3-28 17:37 作者: 斑駁 時(shí)間: 2025-3-28 20:39
https://doi.org/10.1007/978-3-322-99087-7h to trigger the type of motion suggested by some workers. It is envisioned that the present-day deformation of the Aegean is a response to vertical movement of lithothermal masses rather than to horizontal deformation and subduction.作者: 豎琴 時(shí)間: 2025-3-28 22:59
Geophysics and Geodynamic Implications for the Evolution of the Hellenidesh to trigger the type of motion suggested by some workers. It is envisioned that the present-day deformation of the Aegean is a response to vertical movement of lithothermal masses rather than to horizontal deformation and subduction.作者: 鋪?zhàn)?nbsp; 時(shí)間: 2025-3-29 04:16
Book 1985 intricate pieces, many of which are already in place. A general image, in terms of science, has emerged, although at this time large gaps are noted and some areas of the picture remain fuzzy and indistinct. In recent years this fascinating, mind-teasing puzzle image has become clearer with individu作者: guardianship 時(shí)間: 2025-3-29 07:17
Geological Information from Satellite Surveys of the Mediterranean Regionns for a given region, but it is necessary to “field check” any area for which lineament maps are prepared. It is critical that such studies be carried out within known morphotectonic regions or smaller domains in which geologic parameters are similar.作者: 值得 時(shí)間: 2025-3-29 14:13
Seismicity of the Mediterranean Basinan and the closing of the Mediterranean Sea. Main tectonic features are of compressive character, with only very localized zones undergoing horizontal tension. The oceanic crust of the Mediterranean Basin is divided into two parts by the Italian peninsula, with the western part belonging to the Eurasian plate and the eastern to the African plate.作者: Omniscient 時(shí)間: 2025-3-29 19:26
Tectonic Evolution of the Tyrrhenian Seail the present a process of oceanization by mantle diapirism took place in the Tyrrhenian area associated with an extensional tectonic regime oriented east-west. The consequent isostatic foundering produced the Tyrrhenian Sea and governed its progressive deepening.作者: Callus 時(shí)間: 2025-3-29 23:20
https://doi.org/10.1007/978-3-662-41335-7Extension of the crystalline basement away from the coasts can be followed by DRS and aeromagnetism. The crust-to-mantle transition is not always evident, and can be a progressive one; prevailing tension fractured the crust and fostered magmatic intrusions and effusions as revealed by magnetic anomalies.作者: 懶鬼才會(huì)衰弱 時(shí)間: 2025-3-30 00:45
https://doi.org/10.1007/978-3-642-92281-7ian Basin. Such kinematics and chronology are consistent with pa-leomagnetic data supporting the Sardinian rotation, basin and margin structure, subsidence since 21 m.y, (especially during Messinian time), and heat flow measurements.作者: Bucket 時(shí)間: 2025-3-30 04:04
,Orientierung über die Elektronentheorie,ont) foreland basements, respectively. The eastern, seismically active front is believed to have resulted from a process of Neogene Apenninization of the previous Alpine fold structures, triggered by the eastward migration of domal uplifts, transient in time and space.作者: FUSE 時(shí)間: 2025-3-30 09:57
https://doi.org/10.1007/978-3-642-91067-8t of the Adriatic, the Argille del Santerno Formation is widespread; this formation accumulated in platform to slope and basinal environments. Pleistocene biostratigraphy is based on both planktonic and benthonic foraminifera, and we chose . to identify the Neogene-Quaternary boundary.作者: engrave 時(shí)間: 2025-3-30 14:15
Die neueste Entwicklung der Wasserhaltung,per Sirte Slope, where sedimentation commenced in the Upper Cretaceous), comprise a thick to very thick sedimentary sequence that includes deposition from the Triassic to the Quaternary. The Sirte Rise and other geological provinces in the studied area were stretched considerably during the third extensional phase of the Middle-Upper Cretaceous.作者: 愉快嗎 時(shí)間: 2025-3-30 20:33
https://doi.org/10.1007/978-3-0348-4168-9ithospheric slab that developed, during the Tertiary, from the Apennines to the North African orogenic belt. Analysis of the volcano-tectonic evolution also helps establish the relationship between convergent plate tectonics and mantle degassing; plate dehydration would have enhanced only calc-alkaline volcanism.作者: 背叛者 時(shí)間: 2025-3-30 23:35
Erratum to: Die Tanninfarbstoffe,ttern of Pliocene sedimentation is the result of relatively slow deposition during continuing subsidence, producing “starved” basin conditions. During Plio-Quaternary time the average rate of subsidence within the basins was about 0.8 m/1000 years.作者: Receive 時(shí)間: 2025-3-31 03:29
Fallstricke neurologischer Methoden,pted basic conditions for evaporite formation, Krull’s (1917) modification of the Ochsenius model (1876) for evaporite basins is still applicable to the genesis of late Miocene (Messinian) Mediterranean evaporites with no further modification required.作者: 不確定 時(shí)間: 2025-3-31 07:31
Geophysical Contribution to Knowledge of the Mediterranean CrustExtension of the crystalline basement away from the coasts can be followed by DRS and aeromagnetism. The crust-to-mantle transition is not always evident, and can be a progressive one; prevailing tension fractured the crust and fostered magmatic intrusions and effusions as revealed by magnetic anomalies.作者: Presbycusis 時(shí)間: 2025-3-31 11:19
The Western Mediterranean Basinian Basin. Such kinematics and chronology are consistent with pa-leomagnetic data supporting the Sardinian rotation, basin and margin structure, subsidence since 21 m.y, (especially during Messinian time), and heat flow measurements.作者: 相信 時(shí)間: 2025-3-31 16:01
Structural Features and Basin Tectonics of the Tyrrhenian Seaont) foreland basements, respectively. The eastern, seismically active front is believed to have resulted from a process of Neogene Apenninization of the previous Alpine fold structures, triggered by the eastward migration of domal uplifts, transient in time and space.
