A 3D organized point cloud clustering algorithm for seismic fault data based on region growth
Abstract Traditional classification methods for seismic fault 3D point cloud data rely on fault annotation data. Fault annotation data is usually stored in the data structure of a 3D array, and represented by organized point cloud data. The artificial fault annotation method analyses point data in e...
Ausführliche Beschreibung
Autor*in: |
Zhao, Lihong [verfasserIn] |
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E-Artikel |
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Sprache: |
Englisch |
Erschienen: |
2023 |
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Anmerkung: |
© The Author(s), under exclusive licence to Springer Nature Switzerland AG 2023. Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law. |
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Übergeordnetes Werk: |
Enthalten in: Computational geosciences - New York, NY [u.a.] : Springer Science + Business Media B.V., 1997, 27(2023), 6 vom: 26. Okt., Seite 1165-1181 |
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Übergeordnetes Werk: |
volume:27 ; year:2023 ; number:6 ; day:26 ; month:10 ; pages:1165-1181 |
Links: |
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DOI / URN: |
10.1007/s10596-023-10259-6 |
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Katalog-ID: |
SPR053985125 |
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520 | |a Abstract Traditional classification methods for seismic fault 3D point cloud data rely on fault annotation data. Fault annotation data is usually stored in the data structure of a 3D array, and represented by organized point cloud data. The artificial fault annotation method analyses point data in each 2D slice respectively, without considering the 3D spatial distribution of all points, produces results without clustering and proper continuity in 3D space, and causes inconvenience for subsequent research work, such as calculation of the trend, inclination, and other information of each single fault. This paper presents a very simple but efficient clustering method for seismic fault annotation point cloud data to divide the points into each fault. To provide features as fundaments for this clustering method, we propose a normal direction estimation algorithm for seismic fault point cloud data. Tested by the experiments on synthetic data and field data, our method can divide the points with accuracy, reliability, and adaptability, thus providing a foundation for unified analysis, processing, and calculation for each part of the same fault, and analyzing fault displacement and low sequence faults, moreover, the clustering result could be used to fix 3D continuity of fault annotation data itself. | ||
520 | |a Highlights Directly analysis of organized point cloud to clustering faults.Proposes an efficient and reliable fault feature extraction and analysis algorithm.Directly analyze the original fault annotation 3D point cloud without approximation. | ||
650 | 4 | |a Fault clustering |7 (dpeaa)DE-He213 | |
650 | 4 | |a Normal estimation |7 (dpeaa)DE-He213 | |
650 | 4 | |a Point cloud |7 (dpeaa)DE-He213 | |
650 | 4 | |a Fault annotation data |7 (dpeaa)DE-He213 | |
700 | 1 | |a Cai, Minghao |4 aut | |
700 | 1 | |a Ding, Renwei |0 (orcid)0000-0001-7845-1424 |4 aut | |
700 | 1 | |a Zhang, Yujie |4 aut | |
700 | 1 | |a Zhao, Shuo |4 aut | |
700 | 1 | |a Zhang, Jinwei |4 aut | |
700 | 1 | |a Yang, Jing |4 aut | |
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10.1007/s10596-023-10259-6 doi (DE-627)SPR053985125 (SPR)s10596-023-10259-6-e DE-627 ger DE-627 rakwb eng Zhao, Lihong verfasserin aut A 3D organized point cloud clustering algorithm for seismic fault data based on region growth 2023 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © The Author(s), under exclusive licence to Springer Nature Switzerland AG 2023. Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law. Abstract Traditional classification methods for seismic fault 3D point cloud data rely on fault annotation data. Fault annotation data is usually stored in the data structure of a 3D array, and represented by organized point cloud data. The artificial fault annotation method analyses point data in each 2D slice respectively, without considering the 3D spatial distribution of all points, produces results without clustering and proper continuity in 3D space, and causes inconvenience for subsequent research work, such as calculation of the trend, inclination, and other information of each single fault. This paper presents a very simple but efficient clustering method for seismic fault annotation point cloud data to divide the points into each fault. To provide features as fundaments for this clustering method, we propose a normal direction estimation algorithm for seismic fault point cloud data. Tested by the experiments on synthetic data and field data, our method can divide the points with accuracy, reliability, and adaptability, thus providing a foundation for unified analysis, processing, and calculation for each part of the same fault, and analyzing fault displacement and low sequence faults, moreover, the clustering result could be used to fix 3D continuity of fault annotation data itself. Highlights Directly analysis of organized point cloud to clustering faults.Proposes an efficient and reliable fault feature extraction and analysis algorithm.Directly analyze the original fault annotation 3D point cloud without approximation. Fault clustering (dpeaa)DE-He213 Normal estimation (dpeaa)DE-He213 Point cloud (dpeaa)DE-He213 Fault annotation data (dpeaa)DE-He213 Cai, Minghao aut Ding, Renwei (orcid)0000-0001-7845-1424 aut Zhang, Yujie aut Zhao, Shuo aut Zhang, Jinwei aut Yang, Jing aut Enthalten in Computational geosciences New York, NY [u.a.] : Springer Science + Business Media B.V., 1997 27(2023), 6 vom: 26. Okt., Seite 1165-1181 (DE-627)312901313 (DE-600)2001545-8 1573-1499 nnns volume:27 year:2023 number:6 day:26 month:10 pages:1165-1181 https://dx.doi.org/10.1007/s10596-023-10259-6 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 27 2023 6 26 10 1165-1181 |
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10.1007/s10596-023-10259-6 doi (DE-627)SPR053985125 (SPR)s10596-023-10259-6-e DE-627 ger DE-627 rakwb eng Zhao, Lihong verfasserin aut A 3D organized point cloud clustering algorithm for seismic fault data based on region growth 2023 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © The Author(s), under exclusive licence to Springer Nature Switzerland AG 2023. Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law. Abstract Traditional classification methods for seismic fault 3D point cloud data rely on fault annotation data. Fault annotation data is usually stored in the data structure of a 3D array, and represented by organized point cloud data. The artificial fault annotation method analyses point data in each 2D slice respectively, without considering the 3D spatial distribution of all points, produces results without clustering and proper continuity in 3D space, and causes inconvenience for subsequent research work, such as calculation of the trend, inclination, and other information of each single fault. This paper presents a very simple but efficient clustering method for seismic fault annotation point cloud data to divide the points into each fault. To provide features as fundaments for this clustering method, we propose a normal direction estimation algorithm for seismic fault point cloud data. Tested by the experiments on synthetic data and field data, our method can divide the points with accuracy, reliability, and adaptability, thus providing a foundation for unified analysis, processing, and calculation for each part of the same fault, and analyzing fault displacement and low sequence faults, moreover, the clustering result could be used to fix 3D continuity of fault annotation data itself. Highlights Directly analysis of organized point cloud to clustering faults.Proposes an efficient and reliable fault feature extraction and analysis algorithm.Directly analyze the original fault annotation 3D point cloud without approximation. Fault clustering (dpeaa)DE-He213 Normal estimation (dpeaa)DE-He213 Point cloud (dpeaa)DE-He213 Fault annotation data (dpeaa)DE-He213 Cai, Minghao aut Ding, Renwei (orcid)0000-0001-7845-1424 aut Zhang, Yujie aut Zhao, Shuo aut Zhang, Jinwei aut Yang, Jing aut Enthalten in Computational geosciences New York, NY [u.a.] : Springer Science + Business Media B.V., 1997 27(2023), 6 vom: 26. Okt., Seite 1165-1181 (DE-627)312901313 (DE-600)2001545-8 1573-1499 nnns volume:27 year:2023 number:6 day:26 month:10 pages:1165-1181 https://dx.doi.org/10.1007/s10596-023-10259-6 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 27 2023 6 26 10 1165-1181 |
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10.1007/s10596-023-10259-6 doi (DE-627)SPR053985125 (SPR)s10596-023-10259-6-e DE-627 ger DE-627 rakwb eng Zhao, Lihong verfasserin aut A 3D organized point cloud clustering algorithm for seismic fault data based on region growth 2023 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © The Author(s), under exclusive licence to Springer Nature Switzerland AG 2023. Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law. Abstract Traditional classification methods for seismic fault 3D point cloud data rely on fault annotation data. Fault annotation data is usually stored in the data structure of a 3D array, and represented by organized point cloud data. The artificial fault annotation method analyses point data in each 2D slice respectively, without considering the 3D spatial distribution of all points, produces results without clustering and proper continuity in 3D space, and causes inconvenience for subsequent research work, such as calculation of the trend, inclination, and other information of each single fault. This paper presents a very simple but efficient clustering method for seismic fault annotation point cloud data to divide the points into each fault. To provide features as fundaments for this clustering method, we propose a normal direction estimation algorithm for seismic fault point cloud data. Tested by the experiments on synthetic data and field data, our method can divide the points with accuracy, reliability, and adaptability, thus providing a foundation for unified analysis, processing, and calculation for each part of the same fault, and analyzing fault displacement and low sequence faults, moreover, the clustering result could be used to fix 3D continuity of fault annotation data itself. Highlights Directly analysis of organized point cloud to clustering faults.Proposes an efficient and reliable fault feature extraction and analysis algorithm.Directly analyze the original fault annotation 3D point cloud without approximation. Fault clustering (dpeaa)DE-He213 Normal estimation (dpeaa)DE-He213 Point cloud (dpeaa)DE-He213 Fault annotation data (dpeaa)DE-He213 Cai, Minghao aut Ding, Renwei (orcid)0000-0001-7845-1424 aut Zhang, Yujie aut Zhao, Shuo aut Zhang, Jinwei aut Yang, Jing aut Enthalten in Computational geosciences New York, NY [u.a.] : Springer Science + Business Media B.V., 1997 27(2023), 6 vom: 26. Okt., Seite 1165-1181 (DE-627)312901313 (DE-600)2001545-8 1573-1499 nnns volume:27 year:2023 number:6 day:26 month:10 pages:1165-1181 https://dx.doi.org/10.1007/s10596-023-10259-6 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 27 2023 6 26 10 1165-1181 |
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10.1007/s10596-023-10259-6 doi (DE-627)SPR053985125 (SPR)s10596-023-10259-6-e DE-627 ger DE-627 rakwb eng Zhao, Lihong verfasserin aut A 3D organized point cloud clustering algorithm for seismic fault data based on region growth 2023 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © The Author(s), under exclusive licence to Springer Nature Switzerland AG 2023. Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law. Abstract Traditional classification methods for seismic fault 3D point cloud data rely on fault annotation data. Fault annotation data is usually stored in the data structure of a 3D array, and represented by organized point cloud data. The artificial fault annotation method analyses point data in each 2D slice respectively, without considering the 3D spatial distribution of all points, produces results without clustering and proper continuity in 3D space, and causes inconvenience for subsequent research work, such as calculation of the trend, inclination, and other information of each single fault. This paper presents a very simple but efficient clustering method for seismic fault annotation point cloud data to divide the points into each fault. To provide features as fundaments for this clustering method, we propose a normal direction estimation algorithm for seismic fault point cloud data. Tested by the experiments on synthetic data and field data, our method can divide the points with accuracy, reliability, and adaptability, thus providing a foundation for unified analysis, processing, and calculation for each part of the same fault, and analyzing fault displacement and low sequence faults, moreover, the clustering result could be used to fix 3D continuity of fault annotation data itself. Highlights Directly analysis of organized point cloud to clustering faults.Proposes an efficient and reliable fault feature extraction and analysis algorithm.Directly analyze the original fault annotation 3D point cloud without approximation. Fault clustering (dpeaa)DE-He213 Normal estimation (dpeaa)DE-He213 Point cloud (dpeaa)DE-He213 Fault annotation data (dpeaa)DE-He213 Cai, Minghao aut Ding, Renwei (orcid)0000-0001-7845-1424 aut Zhang, Yujie aut Zhao, Shuo aut Zhang, Jinwei aut Yang, Jing aut Enthalten in Computational geosciences New York, NY [u.a.] : Springer Science + Business Media B.V., 1997 27(2023), 6 vom: 26. Okt., Seite 1165-1181 (DE-627)312901313 (DE-600)2001545-8 1573-1499 nnns volume:27 year:2023 number:6 day:26 month:10 pages:1165-1181 https://dx.doi.org/10.1007/s10596-023-10259-6 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 27 2023 6 26 10 1165-1181 |
allfieldsSound |
10.1007/s10596-023-10259-6 doi (DE-627)SPR053985125 (SPR)s10596-023-10259-6-e DE-627 ger DE-627 rakwb eng Zhao, Lihong verfasserin aut A 3D organized point cloud clustering algorithm for seismic fault data based on region growth 2023 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © The Author(s), under exclusive licence to Springer Nature Switzerland AG 2023. Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law. Abstract Traditional classification methods for seismic fault 3D point cloud data rely on fault annotation data. Fault annotation data is usually stored in the data structure of a 3D array, and represented by organized point cloud data. The artificial fault annotation method analyses point data in each 2D slice respectively, without considering the 3D spatial distribution of all points, produces results without clustering and proper continuity in 3D space, and causes inconvenience for subsequent research work, such as calculation of the trend, inclination, and other information of each single fault. This paper presents a very simple but efficient clustering method for seismic fault annotation point cloud data to divide the points into each fault. To provide features as fundaments for this clustering method, we propose a normal direction estimation algorithm for seismic fault point cloud data. Tested by the experiments on synthetic data and field data, our method can divide the points with accuracy, reliability, and adaptability, thus providing a foundation for unified analysis, processing, and calculation for each part of the same fault, and analyzing fault displacement and low sequence faults, moreover, the clustering result could be used to fix 3D continuity of fault annotation data itself. Highlights Directly analysis of organized point cloud to clustering faults.Proposes an efficient and reliable fault feature extraction and analysis algorithm.Directly analyze the original fault annotation 3D point cloud without approximation. Fault clustering (dpeaa)DE-He213 Normal estimation (dpeaa)DE-He213 Point cloud (dpeaa)DE-He213 Fault annotation data (dpeaa)DE-He213 Cai, Minghao aut Ding, Renwei (orcid)0000-0001-7845-1424 aut Zhang, Yujie aut Zhao, Shuo aut Zhang, Jinwei aut Yang, Jing aut Enthalten in Computational geosciences New York, NY [u.a.] : Springer Science + Business Media B.V., 1997 27(2023), 6 vom: 26. Okt., Seite 1165-1181 (DE-627)312901313 (DE-600)2001545-8 1573-1499 nnns volume:27 year:2023 number:6 day:26 month:10 pages:1165-1181 https://dx.doi.org/10.1007/s10596-023-10259-6 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 27 2023 6 26 10 1165-1181 |
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Zhao, Lihong @@aut@@ Cai, Minghao @@aut@@ Ding, Renwei @@aut@@ Zhang, Yujie @@aut@@ Zhao, Shuo @@aut@@ Zhang, Jinwei @@aut@@ Yang, Jing @@aut@@ |
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Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law.</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Abstract Traditional classification methods for seismic fault 3D point cloud data rely on fault annotation data. Fault annotation data is usually stored in the data structure of a 3D array, and represented by organized point cloud data. 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Zhao, Lihong |
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Zhao, Lihong misc Fault clustering misc Normal estimation misc Point cloud misc Fault annotation data A 3D organized point cloud clustering algorithm for seismic fault data based on region growth |
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A 3D organized point cloud clustering algorithm for seismic fault data based on region growth Fault clustering (dpeaa)DE-He213 Normal estimation (dpeaa)DE-He213 Point cloud (dpeaa)DE-He213 Fault annotation data (dpeaa)DE-He213 |
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3d organized point cloud clustering algorithm for seismic fault data based on region growth |
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A 3D organized point cloud clustering algorithm for seismic fault data based on region growth |
abstract |
Abstract Traditional classification methods for seismic fault 3D point cloud data rely on fault annotation data. Fault annotation data is usually stored in the data structure of a 3D array, and represented by organized point cloud data. The artificial fault annotation method analyses point data in each 2D slice respectively, without considering the 3D spatial distribution of all points, produces results without clustering and proper continuity in 3D space, and causes inconvenience for subsequent research work, such as calculation of the trend, inclination, and other information of each single fault. This paper presents a very simple but efficient clustering method for seismic fault annotation point cloud data to divide the points into each fault. To provide features as fundaments for this clustering method, we propose a normal direction estimation algorithm for seismic fault point cloud data. Tested by the experiments on synthetic data and field data, our method can divide the points with accuracy, reliability, and adaptability, thus providing a foundation for unified analysis, processing, and calculation for each part of the same fault, and analyzing fault displacement and low sequence faults, moreover, the clustering result could be used to fix 3D continuity of fault annotation data itself. Highlights Directly analysis of organized point cloud to clustering faults.Proposes an efficient and reliable fault feature extraction and analysis algorithm.Directly analyze the original fault annotation 3D point cloud without approximation. © The Author(s), under exclusive licence to Springer Nature Switzerland AG 2023. Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law. |
abstractGer |
Abstract Traditional classification methods for seismic fault 3D point cloud data rely on fault annotation data. Fault annotation data is usually stored in the data structure of a 3D array, and represented by organized point cloud data. The artificial fault annotation method analyses point data in each 2D slice respectively, without considering the 3D spatial distribution of all points, produces results without clustering and proper continuity in 3D space, and causes inconvenience for subsequent research work, such as calculation of the trend, inclination, and other information of each single fault. This paper presents a very simple but efficient clustering method for seismic fault annotation point cloud data to divide the points into each fault. To provide features as fundaments for this clustering method, we propose a normal direction estimation algorithm for seismic fault point cloud data. Tested by the experiments on synthetic data and field data, our method can divide the points with accuracy, reliability, and adaptability, thus providing a foundation for unified analysis, processing, and calculation for each part of the same fault, and analyzing fault displacement and low sequence faults, moreover, the clustering result could be used to fix 3D continuity of fault annotation data itself. Highlights Directly analysis of organized point cloud to clustering faults.Proposes an efficient and reliable fault feature extraction and analysis algorithm.Directly analyze the original fault annotation 3D point cloud without approximation. © The Author(s), under exclusive licence to Springer Nature Switzerland AG 2023. Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law. |
abstract_unstemmed |
Abstract Traditional classification methods for seismic fault 3D point cloud data rely on fault annotation data. Fault annotation data is usually stored in the data structure of a 3D array, and represented by organized point cloud data. The artificial fault annotation method analyses point data in each 2D slice respectively, without considering the 3D spatial distribution of all points, produces results without clustering and proper continuity in 3D space, and causes inconvenience for subsequent research work, such as calculation of the trend, inclination, and other information of each single fault. This paper presents a very simple but efficient clustering method for seismic fault annotation point cloud data to divide the points into each fault. To provide features as fundaments for this clustering method, we propose a normal direction estimation algorithm for seismic fault point cloud data. Tested by the experiments on synthetic data and field data, our method can divide the points with accuracy, reliability, and adaptability, thus providing a foundation for unified analysis, processing, and calculation for each part of the same fault, and analyzing fault displacement and low sequence faults, moreover, the clustering result could be used to fix 3D continuity of fault annotation data itself. Highlights Directly analysis of organized point cloud to clustering faults.Proposes an efficient and reliable fault feature extraction and analysis algorithm.Directly analyze the original fault annotation 3D point cloud without approximation. © The Author(s), under exclusive licence to Springer Nature Switzerland AG 2023. Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law. |
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A 3D organized point cloud clustering algorithm for seismic fault data based on region growth |
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https://dx.doi.org/10.1007/s10596-023-10259-6 |
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Cai, Minghao Ding, Renwei Zhang, Yujie Zhao, Shuo Zhang, Jinwei Yang, Jing |
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Cai, Minghao Ding, Renwei Zhang, Yujie Zhao, Shuo Zhang, Jinwei Yang, Jing |
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10.1007/s10596-023-10259-6 |
up_date |
2024-07-03T23:17:08.771Z |
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|
score |
7.400717 |