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Journal articles on the topic 'Submarine geology'

To see the other types of publications on this topic, follow the link: Submarine geology.

Author: Grafiati

Published: 4 June 2021

Last updated: 31 July 2024

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1

Harland, W. Brian, Isobel Geddes, and Paul A. Doubleday. "Chapter 11 Southern Svalbard:Bjørnøya and submarine geology." Geological Society, London, Memoirs 17, no. 1 (1997): 209–26. http://dx.doi.org/10.1144/gsl.mem.1997.017.01.11.

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The area south of Spitsbergen (about 76°31'N) to latitude 74°N, and between longitudes 10°E and 35°E, by which Svalbard was first defined, contains the small island of Bjørnøya (Bear Island, Bären Insel) and the rest is sea (Fig. 11.1).The 500 m isobath conveniently separates the edge of the Barents shelf from the Norwegian Sea Basin which runs south from Spitsbergen between 14° and 16°30'E. To the east, the large shallow area, Spitsbergenbanken, less than 100 m deep, supports Bjørnøya at its southwestern end, extends northeast to Hopen and joins Edge°ya. It is separated from Spitsbergen to the north by the Storfjordyrenna and to the east by Hopendjupet. These submarine valleys appear to drain westwards into the ocean deep with deltaic fronts convex westward.This chapter focuses first on Bjørnøya which though small is a key outcrop in the Barents Sea and distinct in many respects from Spitsbergen being about 250 km distant. The chapter then surveys a little of what is known of the surrounding sub-sea area.Bjørnøya (20 km N-S and 15 km E-W), as the southern outpost of Svalbard, has long been a key to Svalbard geology since it is generally free all year from tight sea ice. But though its location is convenient, its cliffs generally bar access. Indeed there are very few places where landing by other than inflatable dinghy are feasible. After the island had been claimed by a Norwegian syndicate in 1915 mining of Tournaisian coal began in 1916 and exported over 116000

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2

GINSBURG, G. D., and V. A. SOLOVIEV. "Russian Research on Submarine Gas Hydrate Geology." Annals of the New York Academy of Sciences 715, no. 1 Natural Gas H (April 1994): 484–86. http://dx.doi.org/10.1111/j.1749-6632.1994.tb38862.x.

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3

Dobbs, Stephen C., Tim McHargue, Matthew A. Malkowski, Jared T. Gooley, Chayawan Jaikla, Colin J. White, and George E. Hilley. "Are submarine and subaerial drainages morphologically distinct?" Geology 47, no. 11 (September 25, 2019): 1093–97. http://dx.doi.org/10.1130/g46329.1.

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Abstract The qualitative resemblance between terrestrial and submarine branched valley networks has led to speculation that common underlying processes control their formation. However, quantitative comparisons have been impeded by methodological limitations and coarse resolution in marine systems. We analyze channel concavity and steepness indices of 23 terrestrial and 29 submarine catchments to determine whether their profile morphologies are distinct. Statistical comparisons of these quantities demonstrate that concavity indices in submarine systems are, in general, lower than in subaerial systems, and that submarine tributaries are steeper than their associated mainstem. These differences may reflect distinct drainage formation mechanisms and dynamics of submarine sediment gravity flows as compared to overland flow processes.

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4

Maier, Katherine L., Charles K. Paull, David W. Caress, Krystle Anderson, Nora M. Nieminski, Eve Lundsten, Benjamin E. Erwin, Roberto Gwiazda, and Andrea Fildani. "Submarine-fan development revealed by integrated high-resolution datasets from La Jolla Fan, offshore California, U.S.A." Journal of Sedimentary Research 90, no. 5 (May 7, 2020): 468–79. http://dx.doi.org/10.2110/jsr.2020.22.

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ABSTRACT New high-resolution datasets across La Jolla submarine fan, offshore California, illuminate low-relief, down-dip widening conduits emanating from a deep-sea channel that deposited a combination of laterally extensive sand strata seemingly crisscrossed by distributary patterns. Extensive coverage of this sector of the seafloor shows submarine-fan architecture and morphologies essentially different than distributary channelized patterns characteristic of subaerial systems and previous conceptual models of submarine fans. The main La Jolla channel, connected to La Jolla Canyon, loses confinement by widening, decreasing in relief, and developing scoured margins across kilometers-long down-slope and lateral distances. Two scales of distributary patterns are associated with sand-rich deposits down-system from, and outside of, fully formed channels. A larger-scale distributary pattern is identified in backscatter and bathymetry from trains of preferential erosion associated with laterally continuous repetitive steps that extend for kilometers outside channel confinement and may represent net erosional upper-flow-regime transitional bedforms. Smaller-scale distributary backscatter patterns in unconfined sand-rich deposits originate from the wide, low-relief channel. We suggest that the newly imaged La Jolla seascape displays sedimentary features that may be common on deep-sea fans but missed in previous lower resolution studies of submarine fans. Thus, La Jolla provides the basis for integrating previously enigmatic and (or) incomplete images of submarine fans. High-resolution seafloor, subsurface, and sample datasets highlight the importance of channel widening, headward erosion, and unconfined flows in La Jolla submarine-fan development, and may be relevant to other sandy submarine fan systems.

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5

Tarazona, Darwin Mateus, Jorge Prieto, William Murphy, Julian Naranjo Vesga, Daniel Rincon, Carlos Hernandez Munoz, Hernan Madero Pinzon, Anderson Mora Mora, and Mateo Acuña-Uribe. "Submarine landslide susceptibility assessment along the southern convergent margin of the Colombian Caribbean." Leading Edge 42, no. 5 (May 2023): 344–59. http://dx.doi.org/10.1190/tle42050344.1.

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Submarine landslides are a mixture of rock, sediment, and fluids moving downslope due to a slope's initial event of mechanical failure. Submarine landslides play a critical role in shaping the morphology of the seafloor and the transport of sediments from the continental shelf to the continental rise in the southern margin of the Colombian Caribbean. Two fundamental considerations can be highlighted: first, mass transport complexes produced by submarine landslides encompass significant portions of the stratigraphic record; second, these mass movements could affect underwater infrastructure. The mapping of the Southern Caribbean seafloor using 3D seismic surveys and multibeam bathymetry data in an area encompassing 59,471 km2 allowed the identification of 220 submarine landslides with areas ranging between 0.1 and 209 km2. Distinctive characteristics were found for submarine landslides associated with canyon walls, channel-levee systems, tectonically controlled ridges, and the continental shelf break. The analysis of the relationship between submarine landslides and seafloor morphological features made it possible to estimate a mass movement susceptibility map that suggests the following considerations: first, structural ridges and adjacent intraslope subbasins related to the South Caribbean Deformed Belt are more likely to be submarine landslide hazards; second, the continental shelf break and channelized systems produce a moderate submarine landslide hazard potential; and third, deep marine systems with a slope less than 5° show the lowest submarine landslide hazard potential. This work contributes to the understanding of submarine landslides in the study area through the presentation of conceptual diagrams that provide additional visual elements facilitating the level of abstraction necessary for visualizing bathymetric data. Likewise, the mass movement susceptibility map presented herein gives insights for future studies that seek to evaluate geohazards in the southern Colombian Caribbean margin.

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6

Polonia, A., M. H. Cormier, N. Cagatay, G. Bortoluzzi, E. Bonatti, L. Gasperini, L. Seeber, et al. "Exploring submarine earthquake geology in the Marmara Sea." Eos, Transactions American Geophysical Union 83, no. 21 (2002): 229. http://dx.doi.org/10.1029/2002eo000158.

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7

Li, Yuting, and Peter D. Clift. "Controls on grain-size variability in the Holocene fill of the Indus Submarine Canyon." Journal of Sedimentary Research 93, no. 2 (February 8, 2023): 71–87. http://dx.doi.org/10.2110/jsr.2022.038.

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ABSTRACT What processes control grain size and bed thickness in submarine canyon deposits? Erosive, shelf-cutting canyons contrast with accretionary basin-floor submarine fan accretionary channels because the former tightly constrain turbidity flows in deep channels. This study addresses such a deep-water depositional system in the Indus Submarine Canyon using a series of cores collected along the canyon. Grain-size analysis was conducted for turbidite and hemipelagic sediment deposited in the Holocene Indus Submarine Canyon mostly by diffuse, fine-grained turbidity currents and hemipelagic hypopycnal plumes. We investigate the links between sedimentary grain size, bedding thickness, facies, and canyon morphology. Well-sorted silt in layers mostly < 2 cm thick dominates the canyon. Core sites in the canyon located downstream of knickpoints have coarser, less well sorted sediments because of current acceleration in these areas and then the slowing of flows downslope. Sediments fine with increasing height above the canyon thalweg, implying deposition from a turbulent plume head. The great depth of the canyon, caused by the exceptionally wide shelf and steep slope, prevents channel overspill which controls sedimentation and channel form in submarine fans. Thalweg sediment fines down-canyon into the mid canyon, where sediment bypassing is inferred. The thickest turbidites are found in the sinuous lower canyon where the gradient shallows from ∼ 0.7° to 0.3°. However, canyon gradient has little impact on mean grain size, but does correlate with bed thickness. The active canyon channel, located in a channel belt gradually becomes less steep, more meandering, and narrower farther downstream. Sinuosity is an influence on turbidite bedding thickness but does not control grain size, in contrast to the situation in submarine-fan channel–levee complexes. Compared to the well-known, more proximal Monterey Canyon of California the grain sizes are much finer, although both systems show evidence of > 200 m plume heads.

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8

Li, Cheng, Tai Quan Zhou, Sha Sha Jiang, and Jie Kong. "Finite Element Analysis for the Stress Field and Seepage Field Interaction within Qingdao Submarine Tunnel Rockmass." Applied Mechanics and Materials 405-408 (September 2013): 1278–82. http://dx.doi.org/10.4028/www.scientific.net/amm.405-408.1278.

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The submarine geology characteristic for Qingdao submarine tunnel is fracture and fragmentation with smash rock mass and unevenly distributed rock mass strength. The submarine tunnel is excavated in a weathered rock mass containing water. Before the tunnel lining is constructed, it is important to assure the stability and safety for the rock tunnel and tunnel lining structure during construction and operational periods. As the submarine tunnel is under severe condition, the rock mass stabilization is to a large extent to be determined by the underwater seepage effect. It is fundamental to investigate how the seawater interacts with the tunnel rock mass stress field. To investigate the interaction between the rock mass seepage field and the secondary stress field, the nonlinear finite element software ABAQUS is used to analyze the interaction behavior between the rock mass seepage effect and the tunnel secondary stress field. The rock mass seepage field, stress field are analyzed in detail using the numerical simulation method. Also, the distribution of the tunnel rock mass plastic region is obtained. The numerical analysis results provide guidance for the submarine tunnel construction.

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9

Metivier, F., E. Lajeunesse, and M. C. Cacas. "Submarine Canyons in the Bathtub." Journal of Sedimentary Research 75, no. 1 (January 1, 2005): 6–11. http://dx.doi.org/10.2110/jsr.2005.002.

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10

Soloviev, V., and G. D. Ginsburg. "Formation of submarine gas hydrates." Bulletin of the Geological Society of Denmark 41 (March 30, 1994): 86–94. http://dx.doi.org/10.37570/bgsd-1995-41-09.

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Submarine gas hydrates have been discovered in the course of deep-sea drilling (DSDP and ODP) and bottom sampling in many offshore regions. This paper reports on expeditions carried out in the Black, Caspian and Okhotsk Seas. Gas hydrate accumulations were discovered and investigated in all these areas. The data and an analysis of the results of the deep-sea drilling programme suggest that the infiltration of gas-bearing fluids is a necessary condition for gas hydrate accumulation. This is confirmed by geological observations at three scale levels. Firstly, hydrates in cores are usually associated with comparatively coarse-grained, permeable sediments as well as voids and fractures. Secondly, hydrate accumulations are controlled by permeable geological structures, i.e. faults, diapirs, mud volcanos as well as layered sequences. Thirdly, in the worldwide scale, hydrate accumulations are characteristic of continental slopes and rises and intra-continental seas where submarine seepages also are widespread. Both biogenic and catagenic gas may occur, and the gas sources may be located at various distances from the accumulation. Gas hydrates presumably originate from water-dissolved gas. The possibility of a transition from dissolved gas into hydrate is confirmed by experimental data. Shallow gas hydrate accumulations associated with gas-bearing fluid plumes are the most convenient features for the study of submarine hydrate formation in general. These accumulations are known from the Black, Caspian and Okhotsk Seas, the Gulf of Mexico and off northern California.

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11

Gevorkyan, S. G., B. N. Golubov, and Zh Zh Kalantarova. "THE GEOMETRY OF SUBMARINE VOLCANOES." International Geology Review 29, no. 9 (September 1987): 1035–43. http://dx.doi.org/10.1080/00206818709466197.

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12

Du, Xing, Yongfu Sun, Yupeng Song, Zongxiang Xiu, and Zhiming Su. "Submarine Landslide Susceptibility and Spatial Distribution Using Different Unsupervised Machine Learning Models." Applied Sciences 12, no. 20 (October 19, 2022): 10544. http://dx.doi.org/10.3390/app122010544.

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A submarine landslide is a well-known geohazard that can cause significant damage to offshore engineering facilities. Most standard predicting and mapping methods require expert knowledge, supervision, and fieldwork. In this research, the main objective was to analyze the potential of unsupervised machine learning methods and compare the performance of three different unsupervised machine learning models (k-means, spectral clustering, and hierarchical clustering) in modeling the susceptibility of the submarine landslide. Nine groups of geological factors were selected as the input parameters, which were obtained through field surveys. To estimate submarine landslide susceptibility, all input factors were separated into three or four groups based on data features and environmental variables. Finally, the goodness-of-fit and accuracy of models were validated with both internal metrics (Calinski–Harabasz index, silhouette index, and Davies–Bouldin index) and external metrics (existing landslide distribution, hydrodynamic distribution, and liquefication distribution). The findings of k-means, spectral clustering, and hierarchical clustering performed commendably and accurately in forecasting the submarine landslide susceptibility. Spectral clustering has the greatest congruence with environmental geology parameters. Therefore, the unsupervised machine learning model can be used in submarine-landslide-predicting studies, and the spectral clustering method performed best. Furthermore, machine learning can improve submarine landslide mapping in the future with the development of models and the extension of geological data related to submarine landslides.

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13

"Submarine geology and geophysics." Deep Sea Research Part B. Oceanographic Literature Review 39, no. 8 (August 1992): 656–76. http://dx.doi.org/10.1016/s0198-0254(05)80005-6.

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14

"Submarine geology and geophysics." Deep Sea Research Part B. Oceanographic Literature Review 37, no. 1 (January 1990): 32–64. http://dx.doi.org/10.1016/s0198-0254(05)80012-3.

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15

"Submarine geology and geophysics." Deep Sea Research Part B. Oceanographic Literature Review 37, no. 5 (January 1990): 428–59. http://dx.doi.org/10.1016/s0198-0254(05)80024-x.

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16

"Submarine geology and geophysics." Deep Sea Research Part B. Oceanographic Literature Review 38, no. 4 (January 1991): 300–323. http://dx.doi.org/10.1016/s0198-0254(05)80091-3.

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17

"Submarine geology and geophysics." Deep Sea Research Part B. Oceanographic Literature Review 38, no. 2 (January 1991): 124–55. http://dx.doi.org/10.1016/s0198-0254(05)80102-5.

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18

"Submarine geology and geophysics." Deep Sea Research Part B. Oceanographic Literature Review 38, no. 1 (January 1991): 36–63. http://dx.doi.org/10.1016/s0198-0254(05)80113-x.

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19

"Submarine geology and geophysics." Deep Sea Research Part B. Oceanographic Literature Review 38, no. 7 (January 1991): 562–90. http://dx.doi.org/10.1016/s0198-0254(05)80124-4.

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20

"Submarine geology and geophysics." Deep Sea Research Part B. Oceanographic Literature Review 38, no. 12 (January 1991): 1019–36. http://dx.doi.org/10.1016/s0198-0254(05)80131-1.

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21

"Submarine geology and geophysics." Deep Sea Research Part B. Oceanographic Literature Review 37, no. 2 (January 1990): 138–66. http://dx.doi.org/10.1016/s0198-0254(05)80141-4.

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22

"Submarine geology and geophysics." Deep Sea Research Part B. Oceanographic Literature Review 38, no. 3 (January 1991): 225–50. http://dx.doi.org/10.1016/s0198-0254(05)80148-7.

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23

"Submarine geology and geophysics." Deep Sea Research Part B. Oceanographic Literature Review 38, no. 6 (January 1991): 480–99. http://dx.doi.org/10.1016/s0198-0254(05)80158-x.

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24

"Submarine geology and geophysics." Deep Sea Research Part B. Oceanographic Literature Review 39, no. 2 (February 1992): 131–49. http://dx.doi.org/10.1016/s0198-0254(06)80005-1.

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25

"Submarine geology and geophysics." Deep Sea Research Part B. Oceanographic Literature Review 39, no. 3 (March 1992): 221–57. http://dx.doi.org/10.1016/s0198-0254(06)80012-9.

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26

"Submarine geology and geophysics." Deep Sea Research Part B. Oceanographic Literature Review 39, no. 4 (April 1992): 328–63. http://dx.doi.org/10.1016/s0198-0254(06)80019-1.

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27

"Submarine geology and geophysics." Deep Sea Research Part B. Oceanographic Literature Review 39, no. 7 (July 1992): 572–98. http://dx.doi.org/10.1016/s0198-0254(06)80026-9.

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28

"Submarine geology and geophysics." Deep Sea Research Part B. Oceanographic Literature Review 37, no. 4 (January 1990): 312–50. http://dx.doi.org/10.1016/s0198-0254(06)80078-6.

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29

"Submarine geology and geophysics." Deep Sea Research Part B. Oceanographic Literature Review 38, no. 5 (January 1991): 386–413. http://dx.doi.org/10.1016/s0198-0254(06)80089-0.

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30

"Submarine geology and geophysics." Deep Sea Research Part B. Oceanographic Literature Review 38, no. 10 (January 1991): 850–81. http://dx.doi.org/10.1016/s0198-0254(06)80096-8.

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31

"Submarine geology and geophysics." Deep Sea Research Part B. Oceanographic Literature Review 37, no. 3 (January 1990): 242–55. http://dx.doi.org/10.1016/s0198-0254(06)80103-2.

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32

"Submarine geology and geophysics." Deep Sea Research Part B. Oceanographic Literature Review 39, no. 1 (January 1992): 37–67. http://dx.doi.org/10.1016/s0198-0254(06)80128-7.

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33

"Submarine geology and geophysics." Deep Sea Research Part B. Oceanographic Literature Review 38, no. 11 (January 1991): 935–63. http://dx.doi.org/10.1016/s0198-0254(06)80154-8.

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34

"Submarine geology and geophysics." Deep Sea Research Part B. Oceanographic Literature Review 39, no. 6 (June 1992): 495–514. http://dx.doi.org/10.1016/s0198-0254(06)80161-5.

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35

"Submarine geology and geophysics." Deep Sea Research Part B. Oceanographic Literature Review 39, no. 9 (January 1992): 750–77. http://dx.doi.org/10.1016/s0198-0254(06)80596-0.

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36

"Submarine geology and geophysics." Deep Sea Research Part B. Oceanographic Literature Review 39, no. 5 (May 1992): 426–41. http://dx.doi.org/10.1016/s0198-0254(06)80635-7.

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"Submarine geology and geophysics." Deep Sea Research Part B. Oceanographic Literature Review 38, no. 8 (January 1991): 652–72. http://dx.doi.org/10.1016/s0198-0254(06)80678-3.

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"Submarine geology and geophysics." Deep Sea Research Part B. Oceanographic Literature Review 39, no. 11 (November 1992): 938–62. http://dx.doi.org/10.1016/s0198-0254(06)80695-3.

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"Submarine geology and geophysics." Deep Sea Research Part B. Oceanographic Literature Review 39, no. 12 (December 1992): 1016–38. http://dx.doi.org/10.1016/s0198-0254(09)90018-8.

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"Submarine geology and geophysics." Deep Sea Research Part B. Oceanographic Literature Review 37, no. 11 (January 1990): 1012–38. http://dx.doi.org/10.1016/s0198-0254(09)90028-0.

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"Submarine geology and geophysics." Deep Sea Research Part B. Oceanographic Literature Review 37, no. 9 (January 1990): 805–24. http://dx.doi.org/10.1016/s0198-0254(09)90036-x.

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"Submarine geology and geophysics." Deep Sea Research Part B. Oceanographic Literature Review 37, no. 7 (January 1990): 605–35. http://dx.doi.org/10.1016/s0198-0254(09)90046-2.

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"Submarine geology and geophysics." Deep Sea Research Part B. Oceanographic Literature Review 38, no. 9 (January 1991): 749–71. http://dx.doi.org/10.1016/s0198-0254(09)90054-1.

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44

"Submarine geology and geophysics." Deep Sea Research Part B. Oceanographic Literature Review 32, no. 10 (January 1985): 819–48. http://dx.doi.org/10.1016/0198-0254(85)90025-1.

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"Submarine geology and geophysics." Deep Sea Research Part B. Oceanographic Literature Review 32, no. 11 (January 1985): 949–79. http://dx.doi.org/10.1016/0198-0254(85)90040-8.

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"Submarine geology and geophysics." Deep Sea Research Part B. Oceanographic Literature Review 32, no. 3 (January 1985): 186–203. http://dx.doi.org/10.1016/0198-0254(85)90089-5.

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"Submarine geology and geophysics." Deep Sea Research Part B. Oceanographic Literature Review 32, no. 7 (January 1985): 529–54. http://dx.doi.org/10.1016/0198-0254(85)90107-4.

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48

"Submarine geology and geophysics." Deep Sea Research Part B. Oceanographic Literature Review 32, no. 1 (January 1985): 28–46. http://dx.doi.org/10.1016/0198-0254(85)90123-2.

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"Submarine geology and geophysics." Deep Sea Research Part B. Oceanographic Literature Review 36, no. 7 (January 1989): 573–609. http://dx.doi.org/10.1016/0198-0254(89)92631-9.

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"Submarine geology and geophysics." Deep Sea Research Part B. Oceanographic Literature Review 36, no. 12 (January 1989): 1068–86. http://dx.doi.org/10.1016/0198-0254(89)92639-3.

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