Wide-angle seismic data from ocean bottom seismographs, together with gravity and deep marine reflection profiling data along the Vulcan transect in northern Australia, define the crustal-scale features between the Precambrian Australian craton and the Timor Trough.
The near-vertical marine reflection profiles display a wide range of crustal structures that can be associated with both the accretionary Svecofennian orogeny (1.96 1.75 Ga) and the following Subjotnian and Jotnian rift-stages (1.65 1.11 Ga).
This study uses high-resolution marine seismic reflection profiles to delineate the stratigraphic and structural architecture of the deformation front.
This has been probed here with offshore onshore and OBS, Ocean Bottom Seismometer refraction seismics, in addition to coincident MCS, marine multichannel reflection seismic profiles over the whole North Marmara Trough.
The present study will be of significant importance in the design of various types of coastal structures used in the marine environment for reflection and dissipation of wave energy at continental shelves dominated by stratified fluid which is modeled here as a two-layer fluid.
"Marine survey, marine safety.
Marine-based seismic reflection studies of İmren et al. (2001), Le Pichon et al. (2001, 2003) and Demirbağ et al. (2003) and focal mechanism studies by Örgülü and Aktar (2001) and Özalaybey et al. (2002) indicate the presence of a dextral strike-slip fault along the northeastern margin of the basin (Örgülü 2011).
In the nonfiction works Prospero's Cell (1945), Reflections on a Marine Venus (1953), and Bitter Lemons (1957), Durrell describes the Greek islands of Corfu, where he lived with his first wife in 1937 38; Rhodes, where in 1945 46 he acted as press officer to the Allied government; and Cyprus, his home from 1952 to 1956.
The spatial structure of Macrostrat permits geographic ranges to be measured as the proportion of preserved marine sediments, which is a reflection of the area of shallow marine shelves that is occupied by a given genus (Fig. 1B; see Materials and Methods).
In this work we present a multiscale seismic imaging of the Carboneras Fault (i.e. TOPAS, high-resolution multichannel-seismic reflection, and deep penetration multichannel-seismic reflection) carried out during three successive marine cruises, from 2006 to 2010.
The ACFs successfully showed S reflection retrieval from the basement and an S anisotropy of 2%% within marine sediments from differential travel times of the S reflections polarized in various directions.
