EM1‐Signature in the North Fiji Basin: Evidence for Stagnant Slab‐Derived Mantle Upwelling Beneath the Trench‐Distal Back‐Arc Basin

2021 ◽  
Vol 126 (4) ◽  
Author(s):  
Jihye Oh ◽  
Insung Lee ◽  
Finlay M. Stuart ◽  
Munjae Park ◽  
Jonguk Kim
1994 ◽  
Vol 40 (8) ◽  
pp. 690-697 ◽  
Author(s):  
Pascale Durand ◽  
Afeda Benyagoub ◽  
Daniel Prieur

Sulfur-oxidizing bacteria (n = 161) were enriched and isolated from samples of vent water, invertebrates, and chimney rocks collected at two deep-sea hydrothermal vents (2000 m) in back-arc basins from the southwestern Pacific: the North Fiji Basin and the Lau Basin. Several types of heterotrophic sulfur-oxidizing bacteria were repeatedly isolated. They oxidized thiosulfate either to sulfate (acid producing) or to polythionate (base producing). In most of the acid-producing cultures, thiosulfate was transitorily oxidized to polythionate. All of the bacteria were Gram negative, 37% were fermentative, and 88% were denitrifiers or nitrate reducers. Numerical taxonomy and analysis of the G+C content showed that they belong to several genera including Pseudomonas, Acinetobacter, and Vibrio.Key words: hydrothermal vent, culturable thiosulfate-oxidizing bacteria, numerical taxonomy.


1989 ◽  
Vol 170 (3-4) ◽  
pp. 259-277 ◽  
Author(s):  
Philippe Charvis ◽  
Bernard Pelletier

Clay Minerals ◽  
1994 ◽  
Vol 29 (4) ◽  
pp. 681-692 ◽  
Author(s):  
B. Humphreys ◽  
S. J. Kemp ◽  
G. K. Lott ◽  
Bermanto ◽  
D.A. Dharmayanti ◽  
...  

AbstractGrain-coating chlorite cements commonly occur within sandstones of late Middle and Upper Miocene age deposited in the North Sumatra back-arc basin. Chlorites from the Lower Keutapang Member contain Ca (maximum 0.75 wt% oxide) and show textural evidence for direct precipitation on grains. However, crystals are subhedral, showing curved faces and often ragged edges, and show a tendency to merge together. In overlying beds of the Upper Keutapang Member, grain-coating chlorite-smectite (20% smectite) cements display an identical morphology but are more siliceous, have a lower octahedral occupancy and contain higher total (Na + Ca + K). It is proposed that chlorite cements in the Keutapang Formation originated as smectite-rich cement rims whose initial precipitation was related to the breakdown of volcanic detritus in the sediments. Transformation to chlorite occurred subsequently during burial, facilitated by a high geothermal gradient in the back-arc basin.


Geology ◽  
1988 ◽  
Vol 16 (10) ◽  
pp. 925 ◽  
Author(s):  
Jean-Marie Auzende ◽  
Yves Lafoy ◽  
Bruno Marsset

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