scispace - formally typeset
C

C.E. Smith-Duque

Researcher at National Oceanography Centre

Publications -  11
Citations -  724

C.E. Smith-Duque is an academic researcher from National Oceanography Centre. The author has contributed to research in topics: Oceanic crust & Hydrothermal circulation. The author has an hindex of 7, co-authored 11 publications receiving 613 citations. Previous affiliations of C.E. Smith-Duque include National Oceanography Centre, Southampton & Ocean Drilling Program.

Papers
More filters
Journal ArticleDOI

Reconstructing past seawater Mg/Ca and Sr/Ca from mid-ocean ridge flank calcium carbonate veins

TL;DR: Past oceanic Mg/Ca and Sr/Ca ratios are estimated from suites of 1.6- to 170-million-year-old calcium carbonate veins that had precipitated from seawater-derived fluids in ocean ridge flank basalts to indicate that before the Neogene, oceanic Cation ratios were lower than in the modern ocean.
Journal ArticleDOI

Presence of oxygen and aerobic communities from sea floor to basement in deep-sea sediments

Steven D'Hondt, +64 more
- 01 Apr 2015 - 
TL;DR: The depth of oxygen penetration and microbial activity in marine sediments varies by region as mentioned in this paper, and the depth of microbial communities varies with the region of interest, and the microbial communities can be found up to 75 meters below the sea floor.
Journal ArticleDOI

Channelling of hydrothermal fluids during the accretion and evolution of the upper oceanic crust: Sr isotope evidence from ODP Hole 1256D

TL;DR: ODP Hole 1256D in the eastern equatorial Pacific is the first penetration of a complete section of fast spread ocean crust down to the dike-gabbro transition, and only the second borehole to sample in situ sheeted dikes after DSDP Hole 504B as discussed by the authors.
Journal ArticleDOI

Seafloor basalt alteration and chemical change in the ultra thinly sedimented South Pacific

TL;DR: In this article, the authors report detailed petrographic and geochemical analysis of basalt cores from these sites in order to investigate what impact sediment insulation has on seafloor alteration beyond 10-15 Myr of ocean crust formation.