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Power-law Distribution of normal Fault Displacement and Length and Estimation of Extensional Strain due to normal faults:A Case Study of the Sierra de San Miguelito, Mexico

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Acta Geologica Sinica(English Edition) 2005年第1期79卷 36-42页

作者： XUShunshan A.F.NIETO-SAMANIEGO S.A.ALANIZ-ALVAREZ InstitutoMexicanodelPetrǒleo ProgramaYNFEjeCentralLázaroCárdenasNo.152Col.SanBartoloAtepehuacánC.P.07730 UniversidadNacionalAutǒnomadeMěxico CentrodegeocienciaApartadoPostal1-74276001QuerětaroQro.Měxoco／／InstituteofGeomechnicsChineseAcademyofGeologicalSciencesBeijing100081China.

The Sierra de San Miguelito is a relatively uplifted area and is constituted by a large amount of silicic volcanic rocks with ages from middle to late Cenozoic. The normal faults of the Sierra de San Miguelito are Domino-style and nearly parallel. The cumulative length and displacement of the faults obey power-law distribution. The fractal dimension of the fault traces is -1.49. Using the multi-line one-dimensional sampling, the calculated exponent of cumulative fault displacements is -0.66. A cumulative curve combining measurements of all four sections yielded a slope of -0.63. The displacement-length plot shows a non-linear relationship and large dispersion of data. The large dispersion in the plot is mainly due to the fault linkage during faulting. An estimation of extensional strain due to the normal faults is ca. 0.1830. The bed extension strain is always less than or equal to the horizontal extension strain. The deformation in the Sierra de San Miguelito occurred near the surface, producing pervasive faults and many faults are too small to appear in maps and sections at common scales. The stretching produced by small faults reach ca. 33% of the total horizontal elongation.

关键词： power-law distribution normal faults small faults finite strain Mexico

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Gravitational Tectonics versus Plate Tectonics in the Himalayan Intermontane Basins: NW Himalaya

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Acta Geologica Sinica(English Edition) 2021年第S01期95卷 3-6页

作者： Afroz Ahmad SHAH Nurhafizah MANAN Department of Geosciences Universiti of Brunei DarussalaamJalan Tungku LinkGadong BE 1410Brunei Darussalam

The intermontane basins are some of the critical regions to investigate the formation,growth,and development of basins during the collisional orogenesis,and in the NW Himalaya several such basins are observed to have ... 详细信息

关键词： gravitational tectonics active tectonics Himalaya normal faults deformation domains

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Satellite Data-based Structural Mapping Reveals Active Panjal Traps Fault(PTF)in Kashmir,NW Himalaya

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Acta Geologica Sinica(English Edition) 2024年第S01期98卷 58-61页

作者： Afroz Ahmad SHAH Muhammad Gazali RACHMAN Anushka VASHISTHA Ajay DASHORA Geosciences Programme Faculty of ScienceUniversity Brunei DarussalamBE1410Brunei Universitas Pembangunan Nasional“Veteran” Yogyakarta 55283Indonesia Department of Civil Engineering Indian Institute of Technology GuwahatiAssam 781039India

Exploring the evidence for unidentified earthquake-causing faults in the orogenic zones,and primarily the interior parts(Shah,2013),has been an ongoing quest for centuries(Willis,1923;Baker et al.,1988;Yeats et al.,1992;Wesnousky et al.,1999;Malik et al.,2010;Coudurier-Curveur et al.,2020;Shah et al.,2020).These faults are potentially dangerous due to their unknown risk and deformation budget,two of the most important aspects of mapping and understanding the vulnerability and hazards associated with active faults.

关键词： gravitational tectonics active tectonics normal faults deformation domains Himalaya

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Gravity Fault Subsidence and Beach Ridges Progradation in Quinta-Cassino (RS) Coastal Plain, Brazil

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Open Journal of Geology 2024年第2期14卷 177-195页

作者： Bruno Silva da Fontoura Adelir José Strieder Iran Carlos Stalliviere Corrêa Paulo Rogério Mendes Alexandre Felipe Bruch Angélica Cirolini Programa de Pós-Graduaç &#227o em Geoci&#234ncias (PPGeo) Instituto de Geoci&#234ncias UFRGS Porto Alegre Brazil Engenharia Geológica Centro de Engenharias UFPel Pra&#231a Domingos Rodrigues 2 Pelotas Brasil HIDROSERV-Serviç os Geológicos e Geofísicos Ltda. Rua Senegal 152 Porto Alegre Brazil Colégio Politécnico UFSM Santa Maria Brasil

Ground penetrating radar (GPR) surveys have being applied to investigate very near-surface stratification of sedimentary units in coastal plains and to define their depositional conditions. This paper presents, however, low-frequency GPR survey to investigate fault-related depositional systems at greater depths. The Quinta-Cassino area in the Rio Grande do Sul Coastal Plain (RGSCP, Brazil) shows a wide strandplain that is made off by very long, continuous, and linear geomorphic features (beach ridges). This strandplain extends for ~70 km southward. The beach ridges show low-angle truncations against the Quinta escarpment, and also truncations in the strandplain. The traditional approach points that RGSCP was developed by juxtaposition of four lagoons/barrier systems as consequence of sea level changes;previous model assumes that no deformational episode occurred in RGSCP. The geophysical and geological surveys carried out in this area showed the existence of listric fault controlling the beach ridges in the escarpments and hanging-wall blocks. The radargrams could distinguish Pleistocene basement unit anticlockwise rotation, thickening of beach ridges radarfacies close to listric normal faults, and horst structures. These deformational features indicate that the extensional zone of a large-scale gravity-driven structure controlled the mechanical subsidence, the Holocene sedimentation and its stratigraphic and geomorphic features in the Quinta-Cassino area to build up an asymmetric delta. The results point to a new approach in dealing with RGSCP Holocene evolution.

关键词： Gravity Tectonics normal faults Ground Penetrating Radar Survey Beach-Ridges Progradation

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