愤愤不平
发表于 2025-3-25 03:25:21
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Bucket
发表于 2025-3-25 08:33:47
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
ODIUM
发表于 2025-3-25 12:25:48
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
环形
发表于 2025-3-25 16:57:54
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notification
发表于 2025-3-25 22:37:00
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丰富
发表于 2025-3-26 04:13:07
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gentle
发表于 2025-3-26 07:03:15
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
Liberate
发表于 2025-3-26 10:12:40
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
有角
发表于 2025-3-26 13:41:06
,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
figure
发表于 2025-3-26 19:59:39
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