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標(biāo)題: Titlebook: Geological Setting, Palaeoenvironment and Archaeology of the Red Sea; Najeeb M.A. Rasul,Ian C.F. Stewart Book 2019 Springer Nature Switzer [打印本頁(yè)]

作者: 固執(zhí)已見(jiàn)    時(shí)間: 2025-3-21 19:37
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書(shū)目名稱Geological Setting, Palaeoenvironment and Archaeology of the Red Sea讀者反饋




書(shū)目名稱Geological Setting, Palaeoenvironment and Archaeology of the Red Sea讀者反饋學(xué)科排名





作者: 留戀    時(shí)間: 2025-3-21 21:58

作者: 密切關(guān)系    時(shí)間: 2025-3-22 03:51

作者: Ingratiate    時(shí)間: 2025-3-22 08:36
,Timing of Extensional Faulting Along the Magma-Poor Central and Northern Red Sea Rift Margin—Transi despite evidence for asymmetric extension and hyperextended crust (Zabargad Island). An in-depth analysis of the timing, spatial distribution, and nature of Red Sea volcanism and its relationship to late Cenozoic extensional faulting should shed light on some of the misconceptions. Voluminous Eocen
作者: 全能    時(shí)間: 2025-3-22 11:12

作者: NOVA    時(shí)間: 2025-3-22 13:58
Oceanization Starts at Depth During Continental Rupturing in the Northern Red Sea,ks recovered in the same area both from an oil well below a thick evaporitic-sedimentary sequence, and from a layered mafic complex exposed on the Brothers Islets. These new data provide constraints on the composition, depth of emplacement and age of early syn-rift magma intrusions into the deep cru
作者: NOVA    時(shí)間: 2025-3-22 20:46
Rifting and Salt Deposition on Continental Margins: Differences and Similarities Between the Red Seimentary basins formed during the Gondwana breakup. The interpretation of these seismic profiles integrated with gravity and magnetic potential field data suggest alternative models for the birth of oceanic basins that evolve from an earlier phase of intracontinental rift, salt deposition and contin
作者: 大包裹    時(shí)間: 2025-3-22 21:58
Plate Motions Around the Red Sea Since the Early Oligocene,early Oligocene) and can be represented by two kinematic stages, characterized by distinct directions of extension and different duration. Deformation associated with rifting was accommodated through the reactivation of the inherited Proterozoic structures. We show that the first stage was character
作者: myopia    時(shí)間: 2025-3-23 01:52
Hydrothermal Prospection in the Red Sea Rift: Geochemical Messages from Basalts,measuring chlorine (Cl) excess in erupted lavas. The Red Sea Rift provides a unique opportunity to study assimilation of hydrothermally altered crust at an ultra-slow spreading ridge (maximum 1.6?cm?yr. full spreading rate) by Cl, due to its saline seawater (40–42‰, cf. 35‰ in open ocean water), the
作者: Frenetic    時(shí)間: 2025-3-23 07:20
,Salt Formation, Accumulation, and Expulsion Processes During Ocean Rifting—New Insight Gained from lt Walls’ and ‘Salt Ridges’), associated?with topographical lows (Deeps), suggest that the Red Sea currently?produces new volumes of brines and solid salts underground. The salt?producing zone is focused around the central rifting axis and?represents about 15% of the entire Red Sea area. The brines
作者: adipose-tissue    時(shí)間: 2025-3-23 10:06
Origin of Submarine Channel North of Hanish Sill, Red Sea,ottom waters passing between the basins form gravity currents. In the southernmost Red Sea, in contrast, an 8?km-wide and 100- to 250-m deep channel lies on the north side of Hanish Sill, in an area where the strongest bottom currents flow southward, associated with winter expulsion of dense saline
作者: 容易做    時(shí)間: 2025-3-23 16:27
Cenozoic Faults and Seismicity in Northwest Saudi Arabia and the Gulf of Aqaba Region,identify the youngest geological faults in the area. These faults have been termed Cenozoic faults, although most are Neogene in age, being younger than 23?Ma. A number of previously unknown structures have been identified. These include a zone of shattered and intensely faulted rocks 25?km wide tha
作者: 教育學(xué)    時(shí)間: 2025-3-23 18:21

作者: FLIP    時(shí)間: 2025-3-23 23:46
Variations in Plio-Pleistocene Deposition in the Red Sea,es in the south and with input of aeolian and fluvial sediments through the Tokar Gap in the Sudanese hills. Otherwise, however, the sediment distribution does not obviously reflect the likely pattern of sediment input (from the positions of wind gaps through the Red Sea hills and fluvial drainage b
作者: 虛構(gòu)的東西    時(shí)間: 2025-3-24 03:10
Pleistocene Coral Reef Terraces on the Saudi Arabian Side of the Gulf of Aqaba, Red Sea,Aqaba. Those bordering the Saudi Arabian sector have received little attention thus far, and are comparatively less known than their counterparts in the Sinai sector of the Gulf and in the Red Sea. As is the rule in the Red Sea region, the best developed marine terrace system is reefal and pertains
作者: 變態(tài)    時(shí)間: 2025-3-24 08:53
Mollusc Fauna Associated with Late Pleistocene Coral Reef Systems of the Saudi Arabian Side of the tified and sampled for macrofossils. Terraces ascribable to the last interglacial, the Marine Isotope Stage 5e (MIS5e, ~125kyr BP), predominate and contain a well preserved fossil legacy of sea life at the time. Molluscs proved to represent the most diverse component in the macrobenthos, overwhelmin
作者: 聯(lián)想記憶    時(shí)間: 2025-3-24 13:56

作者: 使迷醉    時(shí)間: 2025-3-24 15:56
Palaeomagnetism and Geochronology of the Harrats Lunayyir and Khaybar Lava Fields, Saudi Arabia,tudy on volcanic rocks from the Khaybar and Lunayyir Harrats plus a site of sediments deposited below the Miocene rocks in the former area. Progressive thermal or alternating field demagnetization successfully isolated stable characteristic magnetizations (ChRM) that are consistent with a primary ma
作者: 煩躁的女人    時(shí)間: 2025-3-24 21:20

作者: 配偶    時(shí)間: 2025-3-25 02:26
Princip der Untersuchungsmethode,n of mid-ocean ridges. Competing theories for how spreading begins—either by quasi-instantaneous formation of a whole spreading segment or by initiation of spreading at multiple discrete “nodes” separated by thinned continental lithosphere—have been put forward based, until recently, on the observat
作者: 憤憤不平    時(shí)間: 2025-3-25 03:25

作者: Bucket    時(shí)間: 2025-3-25 08:33
Die quantitative Gerbmittelanalyse despite evidence for asymmetric extension and hyperextended crust (Zabargad Island). An in-depth analysis of the timing, spatial distribution, and nature of Red Sea volcanism and its relationship to late Cenozoic extensional faulting should shed light on some of the misconceptions. Voluminous Eocen
作者: ODIUM    時(shí)間: 2025-3-25 12:25
Franz Wever,Walter Koch,Friedrich Strickerabsence of direct observations. Specifically, it is unclear when during the rifting process the segmented nature of magma supply typical of seafloor spreading initiates. We have imaged the mantle beneath the southern Red Sea, Afar and the Main Ethiopian rift using Rayleigh-wave tomography. From this
作者: 環(huán)形    時(shí)間: 2025-3-25 16:57

作者: notification    時(shí)間: 2025-3-25 22:37

作者: 豐富    時(shí)間: 2025-3-26 04:13

作者: gentle    時(shí)間: 2025-3-26 07:03
Die Ausnutzung minderwertiger Brennstoffe,measuring chlorine (Cl) excess in erupted lavas. The Red Sea Rift provides a unique opportunity to study assimilation of hydrothermally altered crust at an ultra-slow spreading ridge (maximum 1.6?cm?yr. full spreading rate) by Cl, due to its saline seawater (40–42‰, cf. 35‰ in open ocean water), the
作者: Liberate    時(shí)間: 2025-3-26 10:12
https://doi.org/10.1007/978-3-642-50917-9lt Walls’ and ‘Salt Ridges’), associated?with topographical lows (Deeps), suggest that the Red Sea currently?produces new volumes of brines and solid salts underground. The salt?producing zone is focused around the central rifting axis and?represents about 15% of the entire Red Sea area. The brines
作者: 有角    時(shí)間: 2025-3-26 13:41
,Das Kochbuch und die neue Haushaltführung,ottom waters passing between the basins form gravity currents. In the southernmost Red Sea, in contrast, an 8?km-wide and 100- to 250-m deep channel lies on the north side of Hanish Sill, in an area where the strongest bottom currents flow southward, associated with winter expulsion of dense saline
作者: figure    時(shí)間: 2025-3-26 19:59
Die Stellung der Frau im Wirtschaftsleben,identify the youngest geological faults in the area. These faults have been termed Cenozoic faults, although most are Neogene in age, being younger than 23?Ma. A number of previously unknown structures have been identified. These include a zone of shattered and intensely faulted rocks 25?km wide tha
作者: aggravate    時(shí)間: 2025-3-26 23:51
https://doi.org/10.1007/978-3-658-41481-8-order differences in crustal thickness between the Arabian Shield in the west and the Arabian Platform in the east. Moho depths generally increase eastward, while crustal thickness varies strongly in the west over the volcanic regions and near the Red Sea. Localized zones of increased P-wave speed
作者: 反抗者    時(shí)間: 2025-3-27 02:20
Nichteintragung des Rechtsnachfolgevermerkeses in the south and with input of aeolian and fluvial sediments through the Tokar Gap in the Sudanese hills. Otherwise, however, the sediment distribution does not obviously reflect the likely pattern of sediment input (from the positions of wind gaps through the Red Sea hills and fluvial drainage b
作者: labile    時(shí)間: 2025-3-27 06:33

作者: 滑動(dòng)    時(shí)間: 2025-3-27 09:40
,Führen und Mitarbeiterkommunikation,tified and sampled for macrofossils. Terraces ascribable to the last interglacial, the Marine Isotope Stage 5e (MIS5e, ~125kyr BP), predominate and contain a well preserved fossil legacy of sea life at the time. Molluscs proved to represent the most diverse component in the macrobenthos, overwhelmin
作者: MAZE    時(shí)間: 2025-3-27 16:13

作者: Trypsin    時(shí)間: 2025-3-27 17:53
Sonderfall: Korrekturvereinbarung,tudy on volcanic rocks from the Khaybar and Lunayyir Harrats plus a site of sediments deposited below the Miocene rocks in the former area. Progressive thermal or alternating field demagnetization successfully isolated stable characteristic magnetizations (ChRM) that are consistent with a primary ma
作者: 怎樣才咆哮    時(shí)間: 2025-3-27 23:03

作者: Capture    時(shí)間: 2025-3-28 05:11

作者: Blemish    時(shí)間: 2025-3-28 10:08

作者: 食品室    時(shí)間: 2025-3-28 11:15

作者: 不怕任性    時(shí)間: 2025-3-28 17:55

作者: 表臉    時(shí)間: 2025-3-28 20:20
https://doi.org/10.1007/978-3-662-41325-8from orthogonal to oblique with respect to the Red Sea coastlines. Importantly, they correlate across the Red Sea, and provide piercing points for a near coast-to-coast palinspastic reconstruction of the Arabian and Nubian Plates along the entire Red Sea. A tight pre-rift fit of the Arabian and Nubi
作者: 鞠躬    時(shí)間: 2025-3-29 02:00

作者: 小教堂    時(shí)間: 2025-3-29 06:05

作者: 莎草    時(shí)間: 2025-3-29 07:30
https://doi.org/10.1007/978-3-531-18892-8axial oceanic cells is either oceanic or it consists of melt-intruded extended continental crust). Gabbros show petrologic and geochemical signatures similar to those of MORB-type gabbroic cumulates and are compatible with their having been emplaced either in a continental or in an oceanic context.
作者: 運(yùn)動(dòng)的我    時(shí)間: 2025-3-29 13:31
https://doi.org/10.1007/978-3-642-47406-4he proximal rifts onshore and in the platform. Basinward, more elusive features are characterized toward the transitional and oceanic crust in divergent margins. This work discusses alternative interpretations for syn-rift successions and salt distribution in regional seismic profiles from the Red S
作者: 宣稱    時(shí)間: 2025-3-29 18:52
Die Ausnutzung minderwertiger Brennstoffe,e in the southern Red Sea and is still active in the northern region. In this time interval, an inherited system of NW–SE structures was reactivated as normal faults accommodating NE–SW extension, while NE–SW Proterozoic structures were reactivated as transfer strike–slip faults. Although no changes
作者: condescend    時(shí)間: 2025-3-29 20:55

作者: 品嘗你的人    時(shí)間: 2025-3-30 01:00

作者: 彩色    時(shí)間: 2025-3-30 05:11
,Das Kochbuch und die neue Haushaltführung,). Although the stronger currents may help to maintain the upper channel morphology, it is unclear how they would have created the channel, nor can modern currents explain the deeper parts of the channel. The channel is straight and runs parallel with the spreading rift to the north, suggesting that
作者: 使激動(dòng)    時(shí)間: 2025-3-30 09:37

作者: ALLEY    時(shí)間: 2025-3-30 16:02

作者: 宇宙你    時(shí)間: 2025-3-30 17:27
Nichteintragung des Rechtsnachfolgevermerkesre elongated sub-parallel with the coast. For the second, Chirp sediment profiler data allow study of finer scale Pleistocene sedimentation around Thetis Deep in the central Red Sea. The data contain a common sequence of reflections, which suggests that hemipelagic sedimentation has been almost unif
作者: stroke    時(shí)間: 2025-3-30 23:49

作者: 尋找    時(shí)間: 2025-3-31 03:16
,Führen und Mitarbeiterkommunikation,served in these MIS5e coral systems. By and large, the MIS5e deposits document former back reef to fore-reef environments and, to a minor degree, beach or mangal settings. The fauna includes also some index-fossils of ecostratigraphic significance for recognizing MIS5e deposits in the Red Sea. The M
作者: 痛打    時(shí)間: 2025-3-31 07:35
Anforderungen an eine wirksame Abmahnung,Ba/Nb and K/La ratios (7–10 and 200–300, respectively) are similar to those of ocean island basalts (OIBs) and with no evidence of crustal assimilation. Fractionations between incompatible trace elements are used to investigate differences in mantle composition and melting conditions in the studied
作者: 緩解    時(shí)間: 2025-3-31 12:18

作者: 驚奇    時(shí)間: 2025-3-31 16:50

作者: CANDY    時(shí)間: 2025-3-31 17:48
Geological Setting, Palaeoenvironment and Archaeology of the Red Sea
作者: 分貝    時(shí)間: 2025-4-1 01:33

作者: orthopedist    時(shí)間: 2025-4-1 05:43
Neotectonics of the Red Sea, Gulf of Suez and Gulf of Aqaba,ly restricted to the Red Sea marine basin itself, and perhaps narrow belts along its shoulders. In the Gulf of Suez there is enough data to show that each of its sub-basins is presently undergoing extension, but in conjunction with differently oriented, sub-regional shallow crustal stress fields. Th
作者: nocturia    時(shí)間: 2025-4-1 08:11

作者: Lipoprotein    時(shí)間: 2025-4-1 10:10
Constraining the Opening of the Red Sea: Evidence from the Neoproterozoic Margins and Cenozoic Magmfrom orthogonal to oblique with respect to the Red Sea coastlines. Importantly, they correlate across the Red Sea, and provide piercing points for a near coast-to-coast palinspastic reconstruction of the Arabian and Nubian Plates along the entire Red Sea. A tight pre-rift fit of the Arabian and Nubi




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