Saeed SoltaniMoghadam, Anooshiravan Ansari, Leila Etemadsaeed, Mohammad Tatar, Meysam Mahmoodabadi
{"title":"利用地震到达时间模式和梯度增强决策树进行地震定位和震级估计","authors":"Saeed SoltaniMoghadam, Anooshiravan Ansari, Leila Etemadsaeed, Mohammad Tatar, Meysam Mahmoodabadi","doi":"10.1016/j.aiig.2025.100149","DOIUrl":null,"url":null,"abstract":"<div><div>We present a machine learning approach for earthquake location and magnitude estimation based on seismic arrival time patterns, using Histogram-Based Gradient Boosting for its high accuracy and computational efficiency. The model is first evaluated using a synthetic earthquake bulletin that simulates realistic network geometry, station-event distributions, and incorporates a 3D velocity model for accurate travel-time computation. Input features include P and S arrival times and amplitudes, while targets consist of location, origin time, magnitude, and uncertainty measures (horizontal and depth errors, azimuthal gap). Model performance is evaluated using <span><math><msup><mrow><mi>R</mi></mrow><mrow><mn>2</mn></mrow></msup></math></span>, Mean Absolute Error (MAE), and Median Absolute Error (MEDAE), demonstrating high accuracy across datasets with varying levels of completeness. Finally, we validate the model using real-world data from the Ahar-Varzaghan 2012 aftershock sequence in NW Iran. The model accurately recovers key spatial patterns of seismicity despite significant missing data, and the results align with previous high-resolution studies. These findings confirm that the proposed method generalizes well beyond synthetic settings and offers a fast, robust alternative for operational seismic networks and rapid hazard assessment.</div></div>","PeriodicalId":100124,"journal":{"name":"Artificial Intelligence in Geosciences","volume":"6 2","pages":"Article 100149"},"PeriodicalIF":4.2000,"publicationDate":"2025-08-11","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Earthquake location and magnitude estimation using seismic arrival times pattern and gradient boosted decision trees\",\"authors\":\"Saeed SoltaniMoghadam, Anooshiravan Ansari, Leila Etemadsaeed, Mohammad Tatar, Meysam Mahmoodabadi\",\"doi\":\"10.1016/j.aiig.2025.100149\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><div>We present a machine learning approach for earthquake location and magnitude estimation based on seismic arrival time patterns, using Histogram-Based Gradient Boosting for its high accuracy and computational efficiency. The model is first evaluated using a synthetic earthquake bulletin that simulates realistic network geometry, station-event distributions, and incorporates a 3D velocity model for accurate travel-time computation. Input features include P and S arrival times and amplitudes, while targets consist of location, origin time, magnitude, and uncertainty measures (horizontal and depth errors, azimuthal gap). Model performance is evaluated using <span><math><msup><mrow><mi>R</mi></mrow><mrow><mn>2</mn></mrow></msup></math></span>, Mean Absolute Error (MAE), and Median Absolute Error (MEDAE), demonstrating high accuracy across datasets with varying levels of completeness. Finally, we validate the model using real-world data from the Ahar-Varzaghan 2012 aftershock sequence in NW Iran. The model accurately recovers key spatial patterns of seismicity despite significant missing data, and the results align with previous high-resolution studies. These findings confirm that the proposed method generalizes well beyond synthetic settings and offers a fast, robust alternative for operational seismic networks and rapid hazard assessment.</div></div>\",\"PeriodicalId\":100124,\"journal\":{\"name\":\"Artificial Intelligence in Geosciences\",\"volume\":\"6 2\",\"pages\":\"Article 100149\"},\"PeriodicalIF\":4.2000,\"publicationDate\":\"2025-08-11\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Artificial Intelligence in Geosciences\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://www.sciencedirect.com/science/article/pii/S2666544125000450\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Artificial Intelligence in Geosciences","FirstCategoryId":"1085","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S2666544125000450","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
Earthquake location and magnitude estimation using seismic arrival times pattern and gradient boosted decision trees
We present a machine learning approach for earthquake location and magnitude estimation based on seismic arrival time patterns, using Histogram-Based Gradient Boosting for its high accuracy and computational efficiency. The model is first evaluated using a synthetic earthquake bulletin that simulates realistic network geometry, station-event distributions, and incorporates a 3D velocity model for accurate travel-time computation. Input features include P and S arrival times and amplitudes, while targets consist of location, origin time, magnitude, and uncertainty measures (horizontal and depth errors, azimuthal gap). Model performance is evaluated using , Mean Absolute Error (MAE), and Median Absolute Error (MEDAE), demonstrating high accuracy across datasets with varying levels of completeness. Finally, we validate the model using real-world data from the Ahar-Varzaghan 2012 aftershock sequence in NW Iran. The model accurately recovers key spatial patterns of seismicity despite significant missing data, and the results align with previous high-resolution studies. These findings confirm that the proposed method generalizes well beyond synthetic settings and offers a fast, robust alternative for operational seismic networks and rapid hazard assessment.