Zobrazeno 1 - 10
of 56
pro vyhledávání: '"N. R. Chapman"'
Autor:
M. Riedel, M. Scherwath, M. Römer, C. K. Paull, E. M. Lundsten, D. Caress, P. G. Brewer, J. W. Pohlman, L. L. Lapham, N. R. Chapman, M. J. Whiticar, G. D. Spence, R. J. Enkin, K. Douglas
Publikováno v:
Frontiers in Earth Science, Vol 10 (2022)
Barkley Canyon is one of the few known sites worldwide with the occurrence of thermogenic gas seepage and formation of structure-II and structure-H gas hydrate mounds on the seafloor. This site is the location of continuous seafloor monitoring as par
Externí odkaz:
https://doaj.org/article/219d4027962a4d00814bd6f4e93a6155
Publikováno v:
Limnology and Oceanography: Methods. 8:155-171
Natural seepage from the seafloor is a worldwide phenomenon but quantitative measurements of gas release are rare, and the entire range of the dynamics of gas release in space, time, and strength remains unclear so far. To mitigate this, the hydroaco
Publikováno v:
Marine Geology. 252:193-206
This paper describes structurally controlled gas seeps and their influence on seafloor morphology at sites within Queen Charlotte Basin (QCB); a sedimentary basin situated offshore British Columbia, western Canada. Numerous surficial and shallow sedi
Publikováno v:
Marine Geology. 239:83-98
A 1.5 km long, 1 km wide and 70–80 m high carbonate mound was identified on the mid-slope region of the subduction accretionary sedimentary prism offshore Vancouver Island ∼ 3.5 km west of Ocean Drilling Program (ODP) Site 889 and Integrated Ocea
Autor:
N. R. Chapman, R. Marrett
Publikováno v:
The Journal of the Acoustical Society of America. 119:3669-3675
Acoustic transients radiated from small magnitude undersea earthquakes were studied in an experiment carried out using a towed horizontal line array operating in the South Fiji Basin. The transient signals consisted of P, S, and T phases, with the T-
Publikováno v:
Annals of the New York Academy of Sciences. 912:65-75
The Cascadia accretionary margin off Vancouver Island is one of the best studied margins world-wide for the determination of in situ properties of marine gas hydrates. Most quantitative information has come from cores and downhole logs of the Ocean D
Publikováno v:
Nature. 420:656-660
Below water depths of about 300 metres, pressure and temperature conditions cause methane to form ice-like crystals of methane hydrate. Marine deposits of methane hydrate are estimated to be large, amassing about 10,000 gigatonnes of carbon, and are
Publikováno v:
The Leading Edge. 20:87-109
This article describes recent work on marine hydrates off western Canada. Natural occurrences of gas hydrates have been reported in the geoscience literature since the early 1970s. Gas hydrates are solid ice-like structures in which gas molecules (la
Publikováno v:
Journal of Computational Acoustics. :295-306
The paper describes a new broadband tomographic matched field method for estimating the geoacoustic properties of a range-dependent shallow water environment. This method is designed for a multiple acoustic element configuration (several sources and
Publikováno v:
Marine Geology. 164:53-68
A bottom simulating reflector (BSR), representing the base of the gas hydrate stability field, was observed over a closely spaced grid of seismic lines on the continental slope of the northern Cascadia margin. A simple conductive model was used to ca