Application of the Fractal Dimension Calculation Technique to Determine the Shape of Selected Monchepluton Intrusion Crystals (NE Fennoscandia)
Thirty-eight samples of minerals from Paleoproterozoic Layered PGE Intrusion Monchepluton, located in NE Fennoscandia, were tested. An automated computational technique was used which involved counting the sides superimposed on vectorized graphics using separated crystal boundaries. The results were...
Published in: | Minerals |
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Main Authors: | , |
Format: | Text |
Language: | English |
Published: |
Multidisciplinary Digital Publishing Institute
2021
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Subjects: | |
Online Access: | https://doi.org/10.3390/min11101140 |
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author | Miłosz Huber Klaudia Stępniewska |
author_facet | Miłosz Huber Klaudia Stępniewska |
author_sort | Miłosz Huber |
collection | MDPI Open Access Publishing |
container_issue | 10 |
container_start_page | 1140 |
container_title | Minerals |
container_volume | 11 |
description | Thirty-eight samples of minerals from Paleoproterozoic Layered PGE Intrusion Monchepluton, located in NE Fennoscandia, were tested. An automated computational technique was used which involved counting the sides superimposed on vectorized graphics using separated crystal boundaries. The results were obtained for olivine, orthopyroxene, clinopyroxene, and plagioclase. On this basis, an interpretation of the mineral box fractal dimension was made, along with an interpretation of its nature in the rock in which it was found. The performed calculations were applied to the sampling positions, and maps of changes in fractal dimensions were prepared. The nature of the minerals studied was correlated with the type of rocks present in Monchepluton. Then, the fractal dimensions were scaled to a percentage scale determining the mean value for the euhedral crystal as 100%, and a map was obtained representing the advancement of secondary processes after summing these data for all four investigated minerals. This method was analyzed and its advantages and limitations shown. |
format | Text |
genre | Fennoscandia |
genre_facet | Fennoscandia |
id | ftmdpi:oai:mdpi.com:/2075-163X/11/10/1140/ |
institution | Open Polar |
language | English |
op_collection_id | ftmdpi |
op_coverage | agris |
op_doi | https://doi.org/10.3390/min11101140 |
op_relation | Crystallography and Physical Chemistry of Minerals & Nanominerals https://dx.doi.org/10.3390/min11101140 |
op_rights | https://creativecommons.org/licenses/by/4.0/ |
op_source | Minerals; Volume 11; Issue 10; Pages: 1140 |
publishDate | 2021 |
publisher | Multidisciplinary Digital Publishing Institute |
record_format | openpolar |
spelling | ftmdpi:oai:mdpi.com:/2075-163X/11/10/1140/ 2025-01-16T21:50:19+00:00 Application of the Fractal Dimension Calculation Technique to Determine the Shape of Selected Monchepluton Intrusion Crystals (NE Fennoscandia) Miłosz Huber Klaudia Stępniewska agris 2021-10-17 application/pdf https://doi.org/10.3390/min11101140 EN eng Multidisciplinary Digital Publishing Institute Crystallography and Physical Chemistry of Minerals & Nanominerals https://dx.doi.org/10.3390/min11101140 https://creativecommons.org/licenses/by/4.0/ Minerals; Volume 11; Issue 10; Pages: 1140 fractal dimension rock-forming minerals Monchepluton NE Fennoscandia Text 2021 ftmdpi https://doi.org/10.3390/min11101140 2023-08-01T02:58:59Z Thirty-eight samples of minerals from Paleoproterozoic Layered PGE Intrusion Monchepluton, located in NE Fennoscandia, were tested. An automated computational technique was used which involved counting the sides superimposed on vectorized graphics using separated crystal boundaries. The results were obtained for olivine, orthopyroxene, clinopyroxene, and plagioclase. On this basis, an interpretation of the mineral box fractal dimension was made, along with an interpretation of its nature in the rock in which it was found. The performed calculations were applied to the sampling positions, and maps of changes in fractal dimensions were prepared. The nature of the minerals studied was correlated with the type of rocks present in Monchepluton. Then, the fractal dimensions were scaled to a percentage scale determining the mean value for the euhedral crystal as 100%, and a map was obtained representing the advancement of secondary processes after summing these data for all four investigated minerals. This method was analyzed and its advantages and limitations shown. Text Fennoscandia MDPI Open Access Publishing Minerals 11 10 1140 |
spellingShingle | fractal dimension rock-forming minerals Monchepluton NE Fennoscandia Miłosz Huber Klaudia Stępniewska Application of the Fractal Dimension Calculation Technique to Determine the Shape of Selected Monchepluton Intrusion Crystals (NE Fennoscandia) |
title | Application of the Fractal Dimension Calculation Technique to Determine the Shape of Selected Monchepluton Intrusion Crystals (NE Fennoscandia) |
title_full | Application of the Fractal Dimension Calculation Technique to Determine the Shape of Selected Monchepluton Intrusion Crystals (NE Fennoscandia) |
title_fullStr | Application of the Fractal Dimension Calculation Technique to Determine the Shape of Selected Monchepluton Intrusion Crystals (NE Fennoscandia) |
title_full_unstemmed | Application of the Fractal Dimension Calculation Technique to Determine the Shape of Selected Monchepluton Intrusion Crystals (NE Fennoscandia) |
title_short | Application of the Fractal Dimension Calculation Technique to Determine the Shape of Selected Monchepluton Intrusion Crystals (NE Fennoscandia) |
title_sort | application of the fractal dimension calculation technique to determine the shape of selected monchepluton intrusion crystals (ne fennoscandia) |
topic | fractal dimension rock-forming minerals Monchepluton NE Fennoscandia |
topic_facet | fractal dimension rock-forming minerals Monchepluton NE Fennoscandia |
url | https://doi.org/10.3390/min11101140 |