scholarly journals Evaluation of the sedimentary environment of the block 102 of Song Hong basin by petrophysics

2015 ◽  
Vol 18 (4) ◽  
pp. 84-101
Author(s):  
Thanh Thi Ngoc Nguyen ◽  
Luan Thi Bui
Keyword(s):  
Spatial Distribution ◽  
Shallow Water ◽  
Marine Environment ◽  
Coastal Plain ◽  
Tidal Flat ◽  
Middle Miocene ◽  
Sedimentary Environment ◽  
Late Oligocene ◽  
Delta Plain

Interpretation of wireline logging data supported to recover the sedimentary environment of block 102 of Song Hong basin. It inchided in determination of the spatial distribution of source, reservoir and cap rocks and an indispensable part in oil exploration of this area. Resulted wireline logging data showed some sedimentary environment units as the following The late Oligocene was delta environment. It was identified as forming delta plain, swamp to lacustrine. The middle Miocene had changed to shallow water marine environment, which formed the shoreface, tidal flat, lagoon and channel. The lower Miocene was aluvial environment that changed into fluvial and coastal plain.

scholarly journals The Early Silurian Sedimentary Environment of Middle-Upper Yangtze: Lithological and Palaeontological Evidence and Impact on Shale Gas Reservoir

Minerals ◽  
2019 ◽  
Vol 9 (8) ◽  
pp. 494 ◽  
Author(s):  
Qu ◽  
Zhu ◽  
Wang ◽  
Shang
Keyword(s):  
Shallow Water ◽  
Deep Water ◽  
Tidal Flat ◽  
Sedimentary Environment ◽  
Gas Diffusion ◽  
Organic Carbon Content ◽  
High Porosity ◽  
Gas Reservoir ◽  
Longmaxi Shale ◽  
Tight Gas Reservoir

The organic-enriched thick shale at the bottom of Longmaxi Formation is laterally continuous distributed and has been proven to be of good production capability in Fuling of Upper Yangtze. Uplifts that developed during the sedimentation influenced the reservoir characteristics by taking control of the sedimentary environment and provenance. The sedimentary environments are mainly deep-water shelf, shallow-water shelf, and tidal flat. By analyzing reservoir characteristic of these three environments, the deep-water shelf, which dominated the early stage of sedimentation, formed a high-quality reservoir with high TOC (Total Organic Carbon) content, porosity, and brittleness, while the environment was maintained around the basin centre until the Early Silurian. The shales deposited under the shallow-water environment were of low porosity because of the increasing calcareous and argillaceous contents. Sediments which formed on the tidal flat were arenaceous and of the lowest TOC content as the organic preservation conditions deteriorated. The good correlation of graptolite abundance and TOC content, and high porosity within graptolite fossils emphasize the importance of palaeontological development. The argillaceous cap over the Longmaxi shale is of good sealing capability, and the continuous sedimentation zone along southern Sichuan–eastern Chongqing is the best optimized hydrocarbon-bearing system. However, a weak interface on the discontinuity is the potential lateral pathway for gas diffusion at Northern Guizhou and Western Hunan, but on the southeast margin where the dark shale and the tidal sandstone contact, it promises to form a tight gas reservoir.

New late Oligocene echinoids from the central Western Cascades of Oregon

1988 ◽  
Vol 62 (6) ◽  
pp. 945-958 ◽  
Author(s):  
Robert A. Linder ◽  
J. Wyatt Durham ◽  
William N. Orr
Keyword(s):  
Shallow Water ◽  
Marine Environment ◽  
Late Oligocene ◽  
Northeastern Pacific ◽  
Shallow Water Sediments ◽  
Stratigraphic Range

The echinoids Salenia cascadensis n. sp., Stomechinus? dissimilaris n. sp., Glyptocidaris sp., Arbacia abiquaensis n. sp., Lytechinus baldwini n. sp., Gagaria crenularis n. sp., and Kewia marquamensis n. sp. occur in the Late Oligocene (Chattian) Scotts Mills Formation near Silverton, Oregon, just north of 45°N latitude. The echinoids occur in shallow-water sediments deposited among basaltic sea stacks along a rockbound, storm-dominated marginal marine environment. Except for Kewia, these occurrences mark a more northerly limit for these genera in the northeastern Pacific and add to their stratigraphic range.

Determination of acoustic waveguide invariant using ships as sources of opportunity in a shallow water marine environment

2016 ◽  
Vol 140 (4) ◽  
pp. 3364-3364
Author(s):  
Christopher M. Verlinden ◽  
Jit Sarkar ◽  
Bruce Cornuelle ◽  
William A. Kuperman
Keyword(s):  
Shallow Water ◽  
Marine Environment ◽  
Acoustic Waveguide ◽  
Waveguide Invariant

scholarly journals Determination of acoustic waveguide invariant using ships as sources of opportunity in a shallow water marine environment

2017 ◽  
Vol 141 (2) ◽  
pp. EL102-EL107 ◽  
Author(s):  
Christopher M. A. Verlinden ◽  
J. Sarkar ◽  
B. D. Cornuelle ◽  
W. A. Kuperman
Keyword(s):  
Shallow Water ◽  
Marine Environment ◽  
Acoustic Waveguide ◽  
Waveguide Invariant

Spatial assemblage structure of shallow-water reef fish in Southwest Australia

2020 ◽  
Vol 649 ◽  
pp. 125-140
Author(s):  
DS Goldsworthy ◽  
BJ Saunders ◽  
JRC Parker ◽  
ES Harvey
Keyword(s):  
Shallow Water ◽  
Reef Fish ◽  
Marine Environment ◽  
Fish Assemblages ◽  
Canopy Cover ◽  
Reef Fishes ◽  
Reef Fish Assemblage ◽  
Reef Type ◽  
Present Distribution ◽  
Southwest Australia

Bioregional categorisation of the Australian marine environment is essential to conserve and manage entire ecosystems, including the biota and associated habitats. It is important that these regions are optimally positioned to effectively plan for the protection of distinct assemblages. Recent climatic variation and changes to the marine environment in Southwest Australia (SWA) have resulted in shifts in species ranges and changes to the composition of marine assemblages. The goal of this study was to determine if the current bioregionalisation of SWA accurately represents the present distribution of shallow-water reef fishes across 2000 km of its subtropical and temperate coastline. Data was collected in 2015 using diver-operated underwater stereo-video surveys from 7 regions between Port Gregory (north of Geraldton) to the east of Esperance. This study indicated that (1) the shallow-water reef fish of SWA formed 4 distinct assemblages along the coast: one Midwestern, one Central and 2 Southern Assemblages; (2) differences between these fish assemblages were primarily driven by sea surface temperature, Ecklonia radiata cover, non-E. radiata (canopy) cover, understorey algae cover, reef type and reef height; and (3) each of the 4 assemblages were characterised by a high number of short-range Australian and Western Australian endemic species. The findings from this study suggest that 4, rather than the existing 3 bioregions would more effectively capture the shallow-water reef fish assemblage patterns, with boundaries having shifted southwards likely associated with ocean warming.

scholarly journals Quantitative Determination of the Surface Distribution of Supported Metal Nanoparticles: A Laser Ablation–ICP–MS Based Approach

Chemosensors ◽  
2021 ◽  
Vol 9 (4) ◽  
pp. 77
Author(s):  
Davide Spanu ◽  
Gilberto Binda ◽  
Marcello Marelli ◽  
Laura Rampazzi ◽  
Sandro Recchia ◽  
...  
Keyword(s):  
Spatial Distribution ◽  
Laser Ablation ◽  
Quantitative Determination ◽  
Metal Nanoparticles ◽  
Total Mass ◽  
Functional Materials ◽  
Metal Extraction ◽  
Ms Analysis ◽  
Icp Ms

A laser ablation–inductively coupled plasma–mass spectrometry (LA–ICP–MS) based method is proposed for the quantitative determination of the spatial distribution of metal nanoparticles (NPs) supported on planar substrates. The surface is sampled using tailored ablation patterns and the data are used to define three-dimensional functions describing the spatial distribution of NPs. The volume integrals of such interpolated surfaces are calibrated to obtain the mass distribution of Ag NPs by correlation with the total mass of metal as determined by metal extraction and ICP–MS analysis. Once this mass calibration is carried out on a sacrificial sample, quantifications can be performed over multiple samples by a simple micro-destructive LA–ICP–MS analysis without requiring the extraction/dissolution of metal NPs. The proposed approach is here tested using a model sample consisting of a low-density polyethylene (LDPE) disk decorated with silver NPs, achieving high spatial resolution over cm2-sized samples and very high sensitivity. The developed method is accordingly a useful analytical tool for applications requiring both the total mass and the spatial distribution of metal NPs to be determined without damaging the sample surface (e.g., composite functional materials and NPs, decorated catalysts or electrodic materials).

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