Results 31 to 40 of about 1,263 (158)
Millions of seafloor pits, not pockmarks, induced by vertebrates in the North Sea
Seabed pockmarks are among the most prominent morphologic structures in the oceans. They are usually interpreted as surface manifestation of hydrocarbon fluids venting from sediments.
Jens Schneider von Deimling +9 more
doaj +1 more source
Abstract Dinosaur fossils from the Isle of Skye (Scotland, UK), particularly the abundant trace fossil record, provide a window into dinosaur evolution during the poorly known Middle Jurassic. Here we present a comprehensive description of the Duntulm tracksite from Cairidh Ghlumaig Bay, using aerial photography to provide whole site maps, catalogue ...
Paige E. dePolo +7 more
wiley +1 more source
Analisis Data Multibeam Echosounder Untuk Mengidentifikasi Pockmark Pada Perairan Waipoga [PDF]
Wilayah pesisir dan lautan Indonesia terkenal dengan kekayaan dan keanekaragaman sumber daya alamnya. Namun, sebagian besar sumber daya ini belum dimanfaatkan secara optimal.
Lestari, Shintya Ayu
core
Poly-phased fluid flow in the giant fossil pockmark of Beauvoisin, SE basin of France
The giant Jurassic-aged pockmark field of Beauvoisin developed in a 800 m wide depression for over 3.4 Ma during the Oxfordian; it formed below about 600 m water depth.
Gay Aurélien +13 more
doaj +1 more source
Robust Underwater Image Classification Using Image Segmentation, CNN, and Dynamic ROI Approximation
Finding classified rectangular regions of interest (ROIs) in underwater images is still a challenge, and more so if the images pose low quality with respect to illumination conditions, sharpness, and noise.
Stefan Bosse, Parth Kasundra
doaj +1 more source
River Sand and Gravel Mining: Global Drivers, Impacts, and Pathways for Sustainable Management
Abstract River sand and gravel are mined worldwide at volumes that now rival their natural replenishment, yet quantitative knowledge of this mining activity and its consequences lags far behind many other global environmental pressures. We synthesize 411 peer‐reviewed studies published since 1974 within a new Driver‐to‐Management Pathway for ...
Edward Park +25 more
wiley +1 more source
Changes in the physical properties of calcareous ooze between intact weak layers and glide planes within the same stratigraphy provide new constraints on the deformation processes and mechanical factors that control the mobility and erosive behaviour of submarine carbonate landslides.
Yan Li +4 more
wiley +1 more source
Location of the three study sites on the Regab pockmark:
Site 1 at the north of the pockmark (Guineco Marker 3), Site 2 at the center of the pockmark (Guineco Marker 7) and Site 3 in the southwestern part of the pockmark (Guineco Marker 10). Images ROV Victor 6000, WACS cruise – Ifremer. Reprinted from Ifremer
Carole Decker (171640) +3 more
core +1 more source
Fluid Pathways and Sources Driving Recurring Pockmark Formation on the Chatham Rise, New Zealand
Quasi‐3D seismic data interpretation and spatial pattern analysis indicate that pockmark formation on the SW Chatham Rise is likely driven by a combination of compaction‐related dewatering during polygonal faulting and silica diagenesis, coupled with deeply‐sourced, possibly CO2‐rich fluids from subducted limestones migrating along prominent basement ...
Fynn Warnke +4 more
wiley +1 more source
ABSTRACT The enigmatic Ediacara biota represents Earth's earliest example of macroscopic, complex life, yet the driving forces promoting their mid‐Ediacaran evolution and subsequent extinction across the Ediacaran–Cambrian boundary remain speculative. If these were true animals requiring oxygen for aerobic respiration, their rise has often been linked ...
Andrew D. Doerrler +10 more
wiley +1 more source

