Matches in SemOpenAlex for { <https://semopenalex.org/work/W4230194580> ?p ?o ?g. }
Showing items 1 to 76 of
76
with 100 items per page.
- W4230194580 endingPage "88" @default.
- W4230194580 startingPage "63" @default.
- W4230194580 abstract "At present two brine-filled depressions have been identified in the eastern Mediterranean - The Tyro Basin (33°53′N, 26°02′E) and the Bannock Basin (34°20′N, 20°02′E). In both areas, the main basin is surrounded by satellite basins that used to have or still have hypersaline and anoxic conditions. The brines are thought to originate from dissolution of outcropping or underlying (Messinian) evaporitic salt layers. The transition from normal seawater to brine water occurs at a slightly different water depth in the two basins; at 3383 dbar in the Tyro Basin and at 3330 dbar in the Bannock Basin. At this transition, salinity increases sharply, whereas the concentration of dissolved oxygen drops rapidly to zero across a depth interval of only a few metres. The brines in the anoxic Tyro and Bannock Basins are of almost identical salinity (10 times that of seawater). However, between the Tyro and Bannock brines differences occur in the major (and trace) element composition. The Tyro brine is characterized by a relatively high Na content, whereas the Bannock brine is more enriched in K, Mg and SO4. These differences are related to the composition of the (Messinian) evaporitic salt that serves as a source for each of these brines. The differences in evaporite composition result from differences in the depositional ‘stage’ of the two salt deposits. The Bannock brine results from dissolution of a late-stage evaporitic salt deposit, whereas the Tyro brine originates from an earlier-stage evaporite. In contrast to the homogeneous brine in the Tyro Basin, a double-layered brine is observed in the Bannock Basin. The lower brine (II) has a slightly higher salinity than the upper brine (I) and the brines also differ in composition. Brine I has a higher concentration of Ca and Sr, and a lower concentration of Mg, S and SO4. The concentrations of these ions in the Scirocco brine deviate even more from those in brine II, which is thought to indicate a higher degree of dolomitization in the Scirocco Basin." @default.
- W4230194580 created "2022-05-11" @default.
- W4230194580 creator A5019235189 @default.
- W4230194580 creator A5031050448 @default.
- W4230194580 creator A5032173361 @default.
- W4230194580 creator A5047236072 @default.
- W4230194580 creator A5053650782 @default.
- W4230194580 creator A5058883714 @default.
- W4230194580 creator A5059908772 @default.
- W4230194580 creator A5078320138 @default.
- W4230194580 date "1990-01-01" @default.
- W4230194580 modified "2023-09-27" @default.
- W4230194580 title "Composition of anoxic hypersaline brines in the Tyro and Bannock Basins, eastern Mediterranean" @default.
- W4230194580 doi "https://doi.org/10.1016/s0304-4203(05)80005-2" @default.
- W4230194580 hasPublicationYear "1990" @default.
- W4230194580 type Work @default.
- W4230194580 citedByCount "0" @default.
- W4230194580 crossrefType "journal-article" @default.
- W4230194580 hasAuthorship W4230194580A5019235189 @default.
- W4230194580 hasAuthorship W4230194580A5031050448 @default.
- W4230194580 hasAuthorship W4230194580A5032173361 @default.
- W4230194580 hasAuthorship W4230194580A5047236072 @default.
- W4230194580 hasAuthorship W4230194580A5053650782 @default.
- W4230194580 hasAuthorship W4230194580A5058883714 @default.
- W4230194580 hasAuthorship W4230194580A5059908772 @default.
- W4230194580 hasAuthorship W4230194580A5078320138 @default.
- W4230194580 hasConcept C108970007 @default.
- W4230194580 hasConcept C109007969 @default.
- W4230194580 hasConcept C111368507 @default.
- W4230194580 hasConcept C127313418 @default.
- W4230194580 hasConcept C129513315 @default.
- W4230194580 hasConcept C151730666 @default.
- W4230194580 hasConcept C17409809 @default.
- W4230194580 hasConcept C178790620 @default.
- W4230194580 hasConcept C185592680 @default.
- W4230194580 hasConcept C197248824 @default.
- W4230194580 hasConcept C199289684 @default.
- W4230194580 hasConcept C2776957854 @default.
- W4230194580 hasConcept C2781113784 @default.
- W4230194580 hasConcept C34221334 @default.
- W4230194580 hasConcept C6494504 @default.
- W4230194580 hasConceptScore W4230194580C108970007 @default.
- W4230194580 hasConceptScore W4230194580C109007969 @default.
- W4230194580 hasConceptScore W4230194580C111368507 @default.
- W4230194580 hasConceptScore W4230194580C127313418 @default.
- W4230194580 hasConceptScore W4230194580C129513315 @default.
- W4230194580 hasConceptScore W4230194580C151730666 @default.
- W4230194580 hasConceptScore W4230194580C17409809 @default.
- W4230194580 hasConceptScore W4230194580C178790620 @default.
- W4230194580 hasConceptScore W4230194580C185592680 @default.
- W4230194580 hasConceptScore W4230194580C197248824 @default.
- W4230194580 hasConceptScore W4230194580C199289684 @default.
- W4230194580 hasConceptScore W4230194580C2776957854 @default.
- W4230194580 hasConceptScore W4230194580C2781113784 @default.
- W4230194580 hasConceptScore W4230194580C34221334 @default.
- W4230194580 hasConceptScore W4230194580C6494504 @default.
- W4230194580 hasIssue "1" @default.
- W4230194580 hasLocation W42301945801 @default.
- W4230194580 hasOpenAccess W4230194580 @default.
- W4230194580 hasPrimaryLocation W42301945801 @default.
- W4230194580 hasRelatedWork W115673260 @default.
- W4230194580 hasRelatedWork W184067610 @default.
- W4230194580 hasRelatedWork W1903691498 @default.
- W4230194580 hasRelatedWork W2001648913 @default.
- W4230194580 hasRelatedWork W2042972130 @default.
- W4230194580 hasRelatedWork W2075842338 @default.
- W4230194580 hasRelatedWork W2132638924 @default.
- W4230194580 hasRelatedWork W2338846363 @default.
- W4230194580 hasRelatedWork W4309609563 @default.
- W4230194580 hasRelatedWork W4316344947 @default.
- W4230194580 hasVolume "31" @default.
- W4230194580 isParatext "false" @default.
- W4230194580 isRetracted "false" @default.
- W4230194580 workType "article" @default.