scholarly journals Sampling of Laminated Beach Sands

10.4138/1790 ◽  
1969 ◽  
Vol 5 (2) ◽  
Author(s):  
Rudolf A. Gees
Keyword(s):  
Beach Sands

TEXTURAL AND GEOCHEMICAL CHARACTERISTICS OF BEACH SANDS ALONG THE WESTERN GULF OF MEXICO, MEXICO

2017 ◽  
Vol 13 (1) ◽  
pp. 161-174 ◽  
Author(s):  
Violeta HERNÁNDEZ-HINOJOSA ◽  
◽  
Patricia C. MONTIEL-GARCÍA ◽  
John S. ARMSTRONG-ALTRIN ◽  
Ramasamy NAGARAJAN ◽  
...  
Keyword(s):  
Gulf Of Mexico ◽  
Geochemical Characteristics ◽  
Beach Sands

scholarly journals Mineralogy, Geochemistry and Provenance of Coastal Sands from Greece: New Insights on the REE Content of Black Coastal Sands from Aggelochori Area, N.-Greece

Minerals ◽  
2021 ◽  
Vol 11 (7) ◽  
pp. 693
Author(s):  
Argyrios Papadopoulos ◽  
Stylianos Lazaridis ◽  
Afroditi Kipourou-Panagiotou ◽  
Nikolaos Kantiranis ◽  
Antonios Koroneos ◽  
...  
Keyword(s):  
Major And Trace Elements ◽  
Heavy Minerals ◽  
Sea Waves ◽  
Complex Flow ◽  
Fine Grained ◽  
Microscopy Analysis ◽  
Beach Sands ◽  
Geochemical Analyses ◽  
The One ◽  
Black Color

Beach sands from Aggelochori coast line are investigated for their geochemistry and REE content, mineralogy and their provenance. These fluvial sands bear heavy minerals enriched horizons (containing minerals such as magnetite, zircon, ilmenite, hematite, rutile and titanite) that can be distinguished due to their black color and are formed usually due to the action of sea waves that deposit the heavy minerals and remove the lighter ones. After a suitable processing (washing, sieving, drying and magnetic separation) of the samples, the mineral constituents and their presence (wt.%) were estimated by XRD. Among the samples, the one being simultaneously the more fine grained and the more zircon-enriched (as suggested by XRPD data and optical microscopy analysis) has been selected for further geochemical analyses. The major and trace elements contents were compared to previously studied REE enriched beach sands from Kavala and Sithonia. Beach sands from Aggelochori area appear to have relatively low REE contents. Considering the provenance of these sediments, we suggest that these sands, are a product of the erosion of multi-sources, including the near-by Monopigado granite, as well as metamorphic rocks, as indicated by the presence of rutile and both ilmenite and magnetite in some samples. Therefore, there are indications of a complex flow pattern that existed at the paleo-catchment area of the deposition.

Postglacial Diatom Stratigraphy in Relation to the Recession of Glacial Lake Agassiz

1975 ◽  
Vol 5 (4) ◽  
pp. 529-540 ◽  
Author(s):  
J.C. Ritchie ◽  
L.K. Koivo
Keyword(s):  
Sandy Beach ◽  
Sedimentary Environment ◽  
Glacial Lake ◽  
Lake Agassiz ◽  
Organic Detritus ◽  
Sedimentary Environments ◽  
Grand Rapids ◽  
Glacial Lake Agassiz ◽  
Diatom Stratigraphy ◽  
Beach Sands

The sediment and diatom stratigraphy of a small pond on The Pas moraine, near Grand Rapids, Manitoba, reveals a change in sedimentary environment related directly to the last stages of Glacial Lake Agassiz. Beach sands were replaced by clay 7300 14C y. a., then by organic silt and, at 4000 14C y. a. by coarse organic detritus; the corresponding diatom assemblages were (I) a predominantly planktonic spectrum in beach sands, (II) a rich assemblage of nonplanktonic forms, and (III) a distinctly nonplanktonic acidophilous spectrum. These results confirm Elson's (1967) reconstruction of the extent and chronology of the final (Pipun) stage of Glacial Lake Agassiz. The sedimentary environments change from a sandy beach of a large lake at 7300 BP to a small, shallow eutrophic pond with clay and silt deposition from 7000 to 4000 BP. From 4000 BP to the present, organic detritus was deposited in a shallow pond that tended toward dystrophy.

Aerial and ground radiometry in relation to the sedimentation of radioactive minerals of the Damietta beach sands, Egypt

1978 ◽  
Vol 73 (8) ◽  
pp. 1738-1748 ◽  
Author(s):  
M. L. Meleik ◽  
K. M. Fouad ◽  
S. N. Wassef ◽  
A. A. Ammar ◽  
G. A. Dabbour
Keyword(s):  
Radioactive Minerals ◽  
Beach Sands

scholarly journals Geochemical maturity of pocket beach sands from the San’in region of southwest Japan

2015 ◽  
Vol 4 (2) ◽  
Author(s):  
Bah Mamadou Lamine Malick ◽  
Hiroaki Ishiga
Keyword(s):  
Southwest Japan ◽  
Beach Sands

scholarly journals Texture and composition of the Rosa Marina beach sands (Adriatic coast, southern Italy): a sedimentological/ecological approach

Geologos ◽  
2016 ◽  
Vol 22 (2) ◽  
pp. 87-103 ◽  
Author(s):  
Massimo Moretti ◽  
Marcello Tropeano ◽  
A.J. (Tom) van Loon ◽  
Pasquale Acquafredda ◽  
Rossella Baldacconi ◽  
...  
Keyword(s):  
Southern Italy ◽  
Statistical Parameters ◽  
Source Areas ◽  
Potential Source ◽  
Physical Study ◽  
Family Level ◽  
Adriatic Coast ◽  
Beach Sands ◽  
Shell Fragments

Abstract Beach sands from the Rosa Marina locality (Adriatic coast, southern Italy) were analysed mainly microscopically in order to trace the source areas of their lithoclastic and bioclastic components. The main cropping out sedimentary units were also studied with the objective to identify the potential source areas of lithoclasts. This allowed to establish how the various rock units contribute to the formation of beach sands. The analysis of the bioclastic components allows to estimate the actual role of organisms regarding the supply of this material to the beach. Identification of taxa that are present in the beach sands as shell fragments or other remains was carried out at the genus or family level. Ecological investigation of the same beach and the recognition of sub-environments (mainly distinguished on the basis of the nature of the substrate and of the water depth) was the key topic that allowed to establish the actual source areas of bioclasts in the Rosa Marina beach sands. The sedimentological analysis (including a physical study of the beach and the calculation of some statistical parameters concerning the grain-size curves) shows that the Rosa Marina beach is nowadays subject to erosion.

scholarly journals Beach sands deposite identification using very low frequency method in the Benteng Lubuk, Krueng Raya coastal area

2021 ◽  
Vol 869 (1) ◽  
pp. 012058
Author(s):  
M Jannah ◽  
M Muhammad ◽  
Marwan ◽  
Z Jalil
Keyword(s):  
Sea Water ◽  
Low Frequency ◽  
High Resistivity ◽  
Conductive Layer ◽  
Inversion Process ◽  
Frequency Method ◽  
Sea Water Intrusion ◽  
Resistive Layer ◽  
Very Low Frequency ◽  
Beach Sands

Abstract The 2D subsurface identification work of iron sands in Benteng Lubuk, Krueng Raya was successfully studied using the very low frequency method based on resistivity mode (VLF-R). This study aims to identify iron sand deposits in coastal areas using electromagnetic inversion. The inversion process shows a conductivity zone of iron sand area, where the resistive layer is strongly covered by a conductive layer above it. High resistivity values were found at 80-100 m stations. This layer has a resistivity value between 20000 – 40000 m and the conductivity value tend to be low. It is estimated that at this point there will only be manifestations of iron sand or sea water intrusion, due to the location of the track close to the coastline.

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