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Strain monitoring of active faults in the central Apennines (Italy) during the period 2002–2017

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F67985831%3A_____%2F19%3A00543661" target="_blank" >RIV/67985831:_____/19:00543661 - isvavai.cz</a>

  • Alternative codes found

    RIV/67985891:_____/19:00509489 RIV/00216208:11310/19:10388552

  • Result on the web

    <a href="https://www.sciencedirect.com/science/article/pii/S0040195118303755" target="_blank" >https://www.sciencedirect.com/science/article/pii/S0040195118303755</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.1016/j.tecto.2018.10.033" target="_blank" >10.1016/j.tecto.2018.10.033</a>

Alternative languages

  • Result language

    angličtina

  • Original language name

    Strain monitoring of active faults in the central Apennines (Italy) during the period 2002–2017

  • Original language description

    We present the results of 3-D monitoring of strain along active faults outcropping in the central Apennines, where recent and historical strong earthquakes occurred, using TM-71 extensometers during the period 2002–2017. We discuss the fault slip development as well as kinematics particularly in the light of local recent seismicity. The recorded fault slip corresponds to the minimum and maximum principal stress with a SW-NE orientation and slightly dipping to SW. Moreover, the detected fault slip is non-linear and affected by remarkable transient periods of acceleration, which lasted up to several months. The recorded accelerations were induced by alternation of extensional, reverse and horizontal displacement due to switching extensional and compressional stress/strain state and coincide with periods of major seismic events that recently affected the central Apennines. This phenomenon is being investigated. In the case of the moderate L'Aquila 2009 and Norcia 2016 earthquakes, the recorded fault slips can be characterized as pre-seismic.

  • Czech name

  • Czech description

Classification

  • Type

    J<sub>imp</sub> - Article in a specialist periodical, which is included in the Web of Science database

  • CEP classification

  • OECD FORD branch

    10505 - Geology

Result continuities

  • Project

    Result was created during the realization of more than one project. More information in the Projects tab.

  • Continuities

    I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Others

  • Publication year

    2019

  • Confidentiality

    S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Data specific for result type

  • Name of the periodical

    Tectonophysics

  • ISSN

    0040-1951

  • e-ISSN

    1879-3266

  • Volume of the periodical

    750

  • Issue of the periodical within the volume

    January

  • Country of publishing house

    NL - THE KINGDOM OF THE NETHERLANDS

  • Number of pages

    14

  • Pages from-to

    22-35

  • UT code for WoS article

    000458713300003

  • EID of the result in the Scopus database

    2-s2.0-85056784748