Carlos Simón Reyes-Martínez , Mario González-Escobar , Juan Carlos Montalvo-Arrieta , Uwe Jenchen , Fernando Velasco-Tapia
{"title":"从墨西卡利山谷二维地震剖面揭示的卡利帕特里亚变形带。古代板块边界的证据?","authors":"Carlos Simón Reyes-Martínez , Mario González-Escobar , Juan Carlos Montalvo-Arrieta , Uwe Jenchen , Fernando Velasco-Tapia","doi":"10.1016/j.tecto.2024.230396","DOIUrl":null,"url":null,"abstract":"<div><p>The geological structures buried in the Mexicali Valley need to be better constrained. The Calipatria Fault is an essential key as it could represent an old strand of the San Andreas Fault system. Previous and two new seismic profiles in the Mexicali Valley and Altar Desert have been processed and interpreted. Chaotic and Low Amplitude Seismic Anomalies (CLASA) observed in the seismic profiles have revealed the Calipatria Deformation Zone, showing a high correlation with gravity maxima. This correlation could extend to the Salton Sea, resulting in an ancient plate boundary connected to the Southern San Andreas Fault. We propose that this deformation zone is a transtension region due to the change from an orthogonal rifting to an oblique rifting similar to the observations on analog models based on the northern Gulf of California. This change in the rifting style produced narrow basins that facilitated continental breakup observed on magnetic anomalies and deep wells penetrating igneous rocks.</p></div>","PeriodicalId":22257,"journal":{"name":"Tectonophysics","volume":"884 ","pages":"Article 230396"},"PeriodicalIF":2.7000,"publicationDate":"2024-06-15","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"The Calipatria Deformation Zone revealed from 2D seismic profiles in the Mexicali Valley. Evidence of an ancient plate boundary?\",\"authors\":\"Carlos Simón Reyes-Martínez , Mario González-Escobar , Juan Carlos Montalvo-Arrieta , Uwe Jenchen , Fernando Velasco-Tapia\",\"doi\":\"10.1016/j.tecto.2024.230396\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><p>The geological structures buried in the Mexicali Valley need to be better constrained. The Calipatria Fault is an essential key as it could represent an old strand of the San Andreas Fault system. Previous and two new seismic profiles in the Mexicali Valley and Altar Desert have been processed and interpreted. Chaotic and Low Amplitude Seismic Anomalies (CLASA) observed in the seismic profiles have revealed the Calipatria Deformation Zone, showing a high correlation with gravity maxima. This correlation could extend to the Salton Sea, resulting in an ancient plate boundary connected to the Southern San Andreas Fault. We propose that this deformation zone is a transtension region due to the change from an orthogonal rifting to an oblique rifting similar to the observations on analog models based on the northern Gulf of California. This change in the rifting style produced narrow basins that facilitated continental breakup observed on magnetic anomalies and deep wells penetrating igneous rocks.</p></div>\",\"PeriodicalId\":22257,\"journal\":{\"name\":\"Tectonophysics\",\"volume\":\"884 \",\"pages\":\"Article 230396\"},\"PeriodicalIF\":2.7000,\"publicationDate\":\"2024-06-15\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Tectonophysics\",\"FirstCategoryId\":\"89\",\"ListUrlMain\":\"https://www.sciencedirect.com/science/article/pii/S0040195124001987\",\"RegionNum\":3,\"RegionCategory\":\"地球科学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q2\",\"JCRName\":\"GEOCHEMISTRY & GEOPHYSICS\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Tectonophysics","FirstCategoryId":"89","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S0040195124001987","RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q2","JCRName":"GEOCHEMISTRY & GEOPHYSICS","Score":null,"Total":0}
The Calipatria Deformation Zone revealed from 2D seismic profiles in the Mexicali Valley. Evidence of an ancient plate boundary?
The geological structures buried in the Mexicali Valley need to be better constrained. The Calipatria Fault is an essential key as it could represent an old strand of the San Andreas Fault system. Previous and two new seismic profiles in the Mexicali Valley and Altar Desert have been processed and interpreted. Chaotic and Low Amplitude Seismic Anomalies (CLASA) observed in the seismic profiles have revealed the Calipatria Deformation Zone, showing a high correlation with gravity maxima. This correlation could extend to the Salton Sea, resulting in an ancient plate boundary connected to the Southern San Andreas Fault. We propose that this deformation zone is a transtension region due to the change from an orthogonal rifting to an oblique rifting similar to the observations on analog models based on the northern Gulf of California. This change in the rifting style produced narrow basins that facilitated continental breakup observed on magnetic anomalies and deep wells penetrating igneous rocks.
期刊介绍:
The prime focus of Tectonophysics will be high-impact original research and reviews in the fields of kinematics, structure, composition, and dynamics of the solid arth at all scales. Tectonophysics particularly encourages submission of papers based on the integration of a multitude of geophysical, geological, geochemical, geodynamic, and geotectonic methods