Results 41 to 50 of about 2,368,102 (348)

Sea Beam Survey of an Active Strike-Slip Fault: The San Clemente Fault in the California Continental Borderland [PDF]

, 1989
The San Clemente fault, located in the California Continental Borderland, is an active, northwest trending, right-lateral, wrench fault. Sea Beam data are used to map the major tectonic landforms associated with active submarine faulting in detail ...
de Moustier, Christian, Legg, Mark R, Luyendyk, Bruce P, Mammerickx, Jacqueline, Tyce, Robert C.   +4 more
core   +2 more sources

Submarine Small-Scale Features of Cyclic Steps in the Penghu Canyon: Implications for the Migration of Canyon

Journal of Marine Science and Engineering, 2022
The submarine canyons are an important clue to study the evolution process of seafloor geomorphology and they generally indicate the significant linear grooves on the seafloor related to seafloor geodynamic erosion during the evolution of geomorphology ...
Shaoyu Zhang, Junjiang Zhu, Yonggang Jia, Sanzhong Li, Ruixue Chen, Xingquan Chen, Xiaolin Ou, Qianqian Li   +7 more
doaj   +1 more source

Research progress on the in-situ monitoring technologies of marine geohazards

Zhongguo dizhi zaihai yu fangzhi xuebao, 2022
Marine geohazards pose a major threat to the population and marine economic development of coastal cities. The expansion of construction of coastal port channels, submarine pipelines, optical cables, and marine platform foundations means that the risk of
Yonggang JIA, Tian CHEN, Peiying LI, Zhenghui LI, Cong HU, Xiaolei LIU, Hongxian SHAN   +6 more
doaj   +1 more source

How to recognize crescentic bedforms formed by supercritical turbidity currents in the geologic record: insights from active submarine channels

, 2018
Submarine channels have been important throughout geologic time for feeding globally significant volumes of sediment from land to the deep sea. Modern observations show that submarine channels can be sculpted by supercritical turbidity currents (seafloor
S. Hage, M. Cartigny, M. Clare, E. Sumner, D. Vendettuoli, J. H. Hughes Clarke, Stephen M. Hubbard, P. Talling, D. Lintern, C. Stacey, Rebecca G. Englert, M. Vardy, J. Hunt, M. Yokokawa, D. Parsons, J. Hizzett, M. Azpiroz-Zabala, A. Vellinga   +17 more
semanticscholar   +1 more source

Exploring the submarine Graham Bank in the Sicily Channel

Annals of Geophysics, 2016
In the Sicily Channel, volcanic activity has been concentrated mainly on the Pantelleria and Linosa islands, while minor submarine volcanism took place in the Adventure, Graham and Nameless banks. The volcanic activity spanned mostly during Plio-Pleistocene, however, historical submarine eruptions occurred in 1831 on the Graham Bank and in 1891 ...
Coltelli M., Cavallaro D., D’Anna G., D'Alessandro A., Grassa F., Mangano G., Patanè D., GRESTA, Stefano   +7 more
openaire   +4 more sources

Sedimentologic and volcanologic investigation of the deep tyrrhenian sea: preliminary result of cruise VST02

Annals of Geophysics, 2006
The VST02 cruise carried out in the summer of 2002 was focused at sedimentologic and volcanologic researches over selected areas of the deep portion of the Tyrrhenian sea.
A. Bertagnini, M. Rosi, D. Penitenti, A. Magagnoli, V. Landuzzi, M. Marani, F. Gamberi, A. Di Roberto   +7 more
doaj   +1 more source

Swath Mapping on the Continental Shelf and Slope: The Eel River Basin, Northern California [PDF]

, 1996
First Paragraph The STRATAFORM program sponsored by the Office of Naval Research (Nittrouer and Kravitz, 1996, this issue) seeks to understand how sedimentary processes lead to the formation of the stratigraphic sequences on continental margins.
Goff, John A., Hughes Clarke, John E, Mayer, Larry A., Pratson, Lincoln F.   +3 more
core   +2 more sources

Mangarara Formation: exhumed remnants of a middle Miocene, temperate carbonate, submarine channel-fan system on the eastern margin of Taranaki Basin, New Zealand [PDF]

, 2009
The middle Miocene Mangarara Formation is a thin (1–60 m), laterally discontinuous unit of moderately to highly calcareous (40–90%) facies of sandy to pure limestone, bioclastic sandstone, and conglomerate that crops out in a few valleys in North ...
Armstrong BD, Betzler C, Beu AG, Gani MR, Harris D, Harris D, Hay RF, Hayward BW, Hornibrook N, Hornibrook N, Hunt D, Hunt TM, Lowe DR, Lowe DR, Martin JM, Nelson CS, Nodder SD, Piper DJW, Posamentier HW, Puga‐Bernabéu A, Reading HG, Ricketts BD, Ruíz‐Ortíz PA, Shanmugam G, Stagpoole V, Wright VP   +25 more
core   +2 more sources

Cell wall target fragment discovery using a low‐cost, minimal fragment library

FEBS Letters, EarlyView.
LoCoFrag100 is a fragment library made up of 100 different compounds. Similarity between the fragments is minimized and 10 different fragments are mixed into a single cocktail, which is soaked to protein crystals. These crystals are analysed by X‐ray crystallography, revealing the binding modes of the bound fragment ligands.
Kaizhou Yan, Mathew Stanley, Olawale Raimi, Andrew T. Ferenbach, Helge C Dorfmueller, Daan M. F. van Aalten   +5 more
wiley   +1 more source

Sedimentary Characteristics and Evolution of the Late Miocene to Quaternary Tributary Channels in the Head of Bounty Channel, New Zealand

Applied Sciences
The Bounty Channel is a large-scale submarine channel system located in the eastern continental margin of New Zealand. Extending along the axis of the Bounty Trough, the channel system comprises three main tributaries (C1–C3) at its head, which merge ...
Xinlan Deng, Ke Huang, Xiang Li
doaj   +1 more source