Analysis of the surface microtextures and morphologies of beach quartz grains in Japan and implications for provenance research

Abstract The mineral quartz is highly resistant to weathering, and various surface microtextures are formed and preserved on quartz grains. These microtextures are considered to reflect the sedimentary history of quartz: parent rock, transportation process, and depositional environment. Thus, quartz...

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Main Authors: Hiromi Itamiya, Ritsuko Sugita, Toshihiko Sugai
Format: Article
Language:English
Published: SpringerOpen 2019-06-01
Series:Progress in Earth and Planetary Science
Subjects:
Online Access:http://link.springer.com/article/10.1186/s40645-019-0287-9
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author Hiromi Itamiya
Ritsuko Sugita
Toshihiko Sugai
author_facet Hiromi Itamiya
Ritsuko Sugita
Toshihiko Sugai
author_sort Hiromi Itamiya
collection DOAJ
description Abstract The mineral quartz is highly resistant to weathering, and various surface microtextures are formed and preserved on quartz grains. These microtextures are considered to reflect the sedimentary history of quartz: parent rock, transportation process, and depositional environment. Thus, quartz grain surface textures have been widely studied for applications in provenance research. This study focuses on beach sediments in Japan that contain various quartz morphologies resulting from the region’s complex geological and geomorphological settings. The goal of the study was to verify the morphological diversity of these quartz grains and reveal the relationship between the quartz morphological features and the sampling site in tectonically active regions. We collected beach sands from backshores in Japan and observed the 15 microtextures of the quartz surfaces using scanning electron microscopy (SEM). The shapes of the quartz grains were also evaluated in terms of roundness parameters based on SEM images. Finally, the particle size distribution and mineral composition of the samples were investigated. The results indicate that quartz roundness can accurately reflect the quartz grain shape and shows a good correlation with the outline observed by SEM. Mechanical features were more frequently observed on the surface of quartz than chemical features. Results show that the coastal areas were under high-energy beach. The coastal sand quartz grains are mainly characterized by (i) v-shaped percussion cracks produced by grain-to-grain collisions in the subaqueous environment and (ii) small holes derived from small inclusion remnants. The v-shaped percussion cracks are related to the sediment source (e.g., a fluvial or marine source), and the holes on the surface are related to the geologic source of the quartz grains. The grain size and mineral composition results support the results of the surface analysis and provide clues regarding sediment provenance. Quartz surface analysis has the potential to show the morphological variation of the coastal sand and provide useful information on the transportation process and parent rock even in areas with complex geological and geomorphological settings such as Japan. The relation between the quartz morphological features and sampling site was based on previous study; however, to develop the analysis, the relation between unweathered quartz shape and parent rock must be clear.
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spelling doaj.art-f31ca1007d6a4859ac21c1ac3c65118c2022-12-22T03:40:37ZengSpringerOpenProgress in Earth and Planetary Science2197-42842019-06-016111410.1186/s40645-019-0287-9Analysis of the surface microtextures and morphologies of beach quartz grains in Japan and implications for provenance researchHiromi Itamiya0Ritsuko Sugita1Toshihiko Sugai2National Research Institute of Police ScienceNational Research Institute of Police ScienceThe University of TokyoAbstract The mineral quartz is highly resistant to weathering, and various surface microtextures are formed and preserved on quartz grains. These microtextures are considered to reflect the sedimentary history of quartz: parent rock, transportation process, and depositional environment. Thus, quartz grain surface textures have been widely studied for applications in provenance research. This study focuses on beach sediments in Japan that contain various quartz morphologies resulting from the region’s complex geological and geomorphological settings. The goal of the study was to verify the morphological diversity of these quartz grains and reveal the relationship between the quartz morphological features and the sampling site in tectonically active regions. We collected beach sands from backshores in Japan and observed the 15 microtextures of the quartz surfaces using scanning electron microscopy (SEM). The shapes of the quartz grains were also evaluated in terms of roundness parameters based on SEM images. Finally, the particle size distribution and mineral composition of the samples were investigated. The results indicate that quartz roundness can accurately reflect the quartz grain shape and shows a good correlation with the outline observed by SEM. Mechanical features were more frequently observed on the surface of quartz than chemical features. Results show that the coastal areas were under high-energy beach. The coastal sand quartz grains are mainly characterized by (i) v-shaped percussion cracks produced by grain-to-grain collisions in the subaqueous environment and (ii) small holes derived from small inclusion remnants. The v-shaped percussion cracks are related to the sediment source (e.g., a fluvial or marine source), and the holes on the surface are related to the geologic source of the quartz grains. The grain size and mineral composition results support the results of the surface analysis and provide clues regarding sediment provenance. Quartz surface analysis has the potential to show the morphological variation of the coastal sand and provide useful information on the transportation process and parent rock even in areas with complex geological and geomorphological settings such as Japan. The relation between the quartz morphological features and sampling site was based on previous study; however, to develop the analysis, the relation between unweathered quartz shape and parent rock must be clear.http://link.springer.com/article/10.1186/s40645-019-0287-9Quartz microtextural analysisProvenance researchSEMInclusionGrain roundnessCoastal sand
spellingShingle Hiromi Itamiya
Ritsuko Sugita
Toshihiko Sugai
Analysis of the surface microtextures and morphologies of beach quartz grains in Japan and implications for provenance research
Progress in Earth and Planetary Science
Quartz microtextural analysis
Provenance research
SEM
Inclusion
Grain roundness
Coastal sand
title Analysis of the surface microtextures and morphologies of beach quartz grains in Japan and implications for provenance research
title_full Analysis of the surface microtextures and morphologies of beach quartz grains in Japan and implications for provenance research
title_fullStr Analysis of the surface microtextures and morphologies of beach quartz grains in Japan and implications for provenance research
title_full_unstemmed Analysis of the surface microtextures and morphologies of beach quartz grains in Japan and implications for provenance research
title_short Analysis of the surface microtextures and morphologies of beach quartz grains in Japan and implications for provenance research
title_sort analysis of the surface microtextures and morphologies of beach quartz grains in japan and implications for provenance research
topic Quartz microtextural analysis
Provenance research
SEM
Inclusion
Grain roundness
Coastal sand
url http://link.springer.com/article/10.1186/s40645-019-0287-9
work_keys_str_mv AT hiromiitamiya analysisofthesurfacemicrotexturesandmorphologiesofbeachquartzgrainsinjapanandimplicationsforprovenanceresearch
AT ritsukosugita analysisofthesurfacemicrotexturesandmorphologiesofbeachquartzgrainsinjapanandimplicationsforprovenanceresearch
AT toshihikosugai analysisofthesurfacemicrotexturesandmorphologiesofbeachquartzgrainsinjapanandimplicationsforprovenanceresearch