Shallow seismic reflection imaging of the Inabanga–Clarin portion of the North Bohol Fault, Central Visayas, Philippines
Abstract On 15 October 2013, a magnitude 7.2 earthquake was generated from a previously unidentified fault in the island of Bohol. This fault was named the North Bohol Fault (NBF) by authorities. We investigated the geometry of the Inabanga–Clarin portion of the NBF using three high-resolution shall...
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| Format: | Article |
| Language: | English |
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SpringerOpen
2019-09-01
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| Series: | Geoscience Letters |
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| Online Access: | http://link.springer.com/article/10.1186/s40562-019-0139-x |
| _version_ | 1818140342214459392 |
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| author | Romer Carlo T. Gacusan Alfredo Mahar Francisco A. Lagmay |
| author_facet | Romer Carlo T. Gacusan Alfredo Mahar Francisco A. Lagmay |
| author_sort | Romer Carlo T. Gacusan |
| collection | DOAJ |
| description | Abstract On 15 October 2013, a magnitude 7.2 earthquake was generated from a previously unidentified fault in the island of Bohol. This fault was named the North Bohol Fault (NBF) by authorities. We investigated the geometry of the Inabanga–Clarin portion of the NBF using three high-resolution shallow seismic reflection profiles to image sections of the fault up to 150 m depth not seen in trenching and regional offshore seismic profiles. These seismic profiles are along the Calubian, Napo, and Caluwasan transects which run perpendicular to the N$$40^{\circ }$$ 40∘ E strike of the NBF. Reverse faults were identified in the Calubian and Napo profiles, whereas a positive flower structure was seen in the Caluwasan profile. Normal faults were also identified in the Caluwasan and Napo profiles. This study corroborates the observations in earlier trenching studies that measured the reverse fault dip angle and direction of the NBF at $$70^{\circ }$$ 70∘ SE. It also demonstrates that topographic flexures are the surface manifestation of steeply dipping faults. The downthrown block of the reverse faults in the Calubian profile defines a depression on the surface; the Napo seismic profile displacement of 3 m is consistent with the 3-m-high surface rupture in Barangay Anonang; and the flower structure in the Caluwasan profile is related to the pressure ridge and right lateral offset stream on the surface. Furthermore, the presence of normal faults as well as the other deformational features is consistent with the transpressional regime described in the literature, wherein the principal horizontal stress is oriented NW–SE. These findings complement earlier geomorphic and trenching investigations of the NBF and demonstrate the application of a tool to image the subsurface and characterize undescribed or hidden faults, which is necessary for earthquake hazard assessment and attendant risk mitigation and prevention planning. |
| first_indexed | 2024-12-11T10:42:27Z |
| format | Article |
| id | doaj.art-76528daf1c064e0ebc42d1fef281891f |
| institution | Directory Open Access Journal |
| issn | 2196-4092 |
| language | English |
| last_indexed | 2024-12-11T10:42:27Z |
| publishDate | 2019-09-01 |
| publisher | SpringerOpen |
| record_format | Article |
| series | Geoscience Letters |
| spelling | doaj.art-76528daf1c064e0ebc42d1fef281891f2022-12-22T01:10:33ZengSpringerOpenGeoscience Letters2196-40922019-09-016111010.1186/s40562-019-0139-xShallow seismic reflection imaging of the Inabanga–Clarin portion of the North Bohol Fault, Central Visayas, PhilippinesRomer Carlo T. Gacusan0Alfredo Mahar Francisco A. Lagmay1National Institute of Geological Sciences, University of the PhilippinesNational Institute of Geological Sciences, University of the PhilippinesAbstract On 15 October 2013, a magnitude 7.2 earthquake was generated from a previously unidentified fault in the island of Bohol. This fault was named the North Bohol Fault (NBF) by authorities. We investigated the geometry of the Inabanga–Clarin portion of the NBF using three high-resolution shallow seismic reflection profiles to image sections of the fault up to 150 m depth not seen in trenching and regional offshore seismic profiles. These seismic profiles are along the Calubian, Napo, and Caluwasan transects which run perpendicular to the N$$40^{\circ }$$ 40∘ E strike of the NBF. Reverse faults were identified in the Calubian and Napo profiles, whereas a positive flower structure was seen in the Caluwasan profile. Normal faults were also identified in the Caluwasan and Napo profiles. This study corroborates the observations in earlier trenching studies that measured the reverse fault dip angle and direction of the NBF at $$70^{\circ }$$ 70∘ SE. It also demonstrates that topographic flexures are the surface manifestation of steeply dipping faults. The downthrown block of the reverse faults in the Calubian profile defines a depression on the surface; the Napo seismic profile displacement of 3 m is consistent with the 3-m-high surface rupture in Barangay Anonang; and the flower structure in the Caluwasan profile is related to the pressure ridge and right lateral offset stream on the surface. Furthermore, the presence of normal faults as well as the other deformational features is consistent with the transpressional regime described in the literature, wherein the principal horizontal stress is oriented NW–SE. These findings complement earlier geomorphic and trenching investigations of the NBF and demonstrate the application of a tool to image the subsurface and characterize undescribed or hidden faults, which is necessary for earthquake hazard assessment and attendant risk mitigation and prevention planning.http://link.springer.com/article/10.1186/s40562-019-0139-xShallow seismic reflectionBohol earthquakeSeismic hazard assessmentSubsurface deformationTranspression |
| spellingShingle | Romer Carlo T. Gacusan Alfredo Mahar Francisco A. Lagmay Shallow seismic reflection imaging of the Inabanga–Clarin portion of the North Bohol Fault, Central Visayas, Philippines Geoscience Letters Shallow seismic reflection Bohol earthquake Seismic hazard assessment Subsurface deformation Transpression |
| title | Shallow seismic reflection imaging of the Inabanga–Clarin portion of the North Bohol Fault, Central Visayas, Philippines |
| title_full | Shallow seismic reflection imaging of the Inabanga–Clarin portion of the North Bohol Fault, Central Visayas, Philippines |
| title_fullStr | Shallow seismic reflection imaging of the Inabanga–Clarin portion of the North Bohol Fault, Central Visayas, Philippines |
| title_full_unstemmed | Shallow seismic reflection imaging of the Inabanga–Clarin portion of the North Bohol Fault, Central Visayas, Philippines |
| title_short | Shallow seismic reflection imaging of the Inabanga–Clarin portion of the North Bohol Fault, Central Visayas, Philippines |
| title_sort | shallow seismic reflection imaging of the inabanga clarin portion of the north bohol fault central visayas philippines |
| topic | Shallow seismic reflection Bohol earthquake Seismic hazard assessment Subsurface deformation Transpression |
| url | http://link.springer.com/article/10.1186/s40562-019-0139-x |
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