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  • 05.09. Miscellaneous  (1)
  • Earthquakes  (1)
  • Friciton, Faults, Longmenshan  (1)
  • 1
    Publication Date: 2021-01-25
    Description: Tectonic pseudotachylytes are solidified frictional melts produced on faults during earthquakes and are robust markers of seismic slip events. Nonetheless, pseudotachylytes are apparently uncommon fault rocks, because they are either rarely produced or are easily lost from the geological record. To solve this conundrum, long-lasting (18–35 days) hydrothermal alteration tests were performed on fresh pseudotachylytes produced by sliding solid rock samples at seismic slip rates in the laboratory. After all tests, the pseudotachylytes were heavily altered with dissolution of the matrix and neo-formation of clay aggregates. Post-alteration products closely resemble natural altered pseudotachylytes and associated ultracataclasites (i.e., fault rocks affected by fracturing in the absence of melting), demonstrating that the preservation potential of original pseudotachylyte microstructures is very short, days to months, in the presence of hydrothermal fluids. As a consequence, pseudotachylytes might be significantly underrepresented in the geological record, and on-fault frictional melting during earthquakes is likely to occur more commonly than generally believed
    Description: ERC CoG NOFEAR 614705
    Description: Published
    Description: e2020GL090020
    Description: 3T. Sorgente sismica
    Description: JCR Journal
    Keywords: Fault ; Earthquakes ; Pseudotachylyte ; Earthquake mechanics
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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  • 2
    Publication Date: 2020-03-03
    Description: All’interno dei percorsi forma vi di Alternanza Scuola­Lavoro un gruppo di ricercatori dell’Istituto Nazionale di Geofisica e Vulcanologia ha proposto e sviluppato con una terza classe del Liceo Scientifico Cavour di Roma un progetto riguardante l’avvicinamento degli studenti al mondo della ricerca scientifica, allo scopo di affrontarla e svilupparla in tu e le sue fasi. Dopo aver spiegato e condiviso l’obiettivo della ricerca con gli alunni, la prima fase del progetto ha riguardato la raccolta dei da tramite l’utilizzo di strumenti di misura; si è in seguito proceduto all’analisi dei dati ottenuti , attraverso un foglio elettronico di calcolo, la produzione di grafici e mappe tema che e infine la scrittura di un articolo scientifico (parte essenziale del lavoro del ricercatore) con la descrizione della ricerca svolta e dei risultati ottenuti . La ricerca ha riguardato la distribuzione del radon indoor in alcuni rioni di Roma. Gli studenti hanno avuto la possibilità di misurare il radon indoor tramite strumenti specifici nelle loro abitazioni e nella loro scuola, di analizzarne la distribuzione spaziale e temporale e di individuare dei casi particolarmente anomali. Sono stati quindi evidenziati i legami tra i valori misura , la geologia del sottosuolo e le tipologie abitative, illustrate per mezzo di mappe tematiche, facendo confluire il tutto o nella scrittura di un articolo scientifico. Il presente rapporto tecnico è stato introdotto dai ricercatori e sviluppato dagli studenti .
    Description: Published
    Description: 1-24
    Description: 1TM. Formazione
    Description: N/A or not JCR
    Keywords: radon ; 05.09. Miscellaneous
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
    Location Call Number Limitation Availability
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  • 3
    Publication Date: 2023-02-09
    Description: The 2008 Mw 7.9 Wenchuan earthquake generated ∼270 and ∼80 km long surface ruptures along the Longmenshan fault belt, namely the Yingxiu-Beichuan fault (YBF) and the Guanxian-Anxian faults (GAF), respectively. So far, most of the frictional investigations were performed on the YBF gouge materials. Here, we present the results of rotary shear friction experiments performed on the GAF gouges recovered from the depth of ∼1.25 km of the Wenchuan Earthquake Fault Scientific Drilling project-3 along the GAF. The fault gouges, mainly composed of quartz, illite, chlorite, and kaolinite, were sheared at slip velocities V ranging from 10−5 to 2 m/s and normal stresses from 8.5 to 10 MPa under both room humidity and wet conditions. At any imposed slip velocity, the wet gouges have an apparent friction coefficient lower than the room humidity one. In addition, enhanced velocity-strengthening behavior at intermediate velocities (10 −2 m/s 〈 V ≤ 10 −1 m/s) was recognized. We characterized the products using field-emission scanning electron microscopy combined with synchrotron X-ray diffraction analysis. These microanalytical investigations evidence the formation of size reduced particles (without mineral phase changes) and R- and Y-shears in the principal slip zone (PSZ). Regardless of the ambient conditions, the width of PSZ was proportional to the input frictional work density (the product of shear stress times displacement). Our results support the hypothesis that the GAF preferentially ruptures through wet fault gouges; however, the enhanced velocity-strengthening regime at intermediate velocities may act as a barrier to slip acceleration during fault rupture propagation.
    Description: This research was financially supported by: (1) the National Natural Science Foundation of China (41830217) (2) the Taiwan ROC (Republic of China) Ministry of Science and Technology (MOST 110-2116-M-008-002-MY2) and Earthquake-Disaster & Risk Evaluation and Management Center (E-DREaM) (3) The Featured Areas Research Center Program within the framework of the Higher Education Sprout Project by the Ministry of Education (MOE), Taiwan, (4) ERC CoG 614705 project NOFEAR
    Description: Published
    Description: e2022JB024081
    Description: 3T. Fisica dei terremoti e Sorgente Sismica
    Description: JCR Journal
    Keywords: Friciton, Faults, Longmenshan ; 04.07. Tectonophysics
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
    Location Call Number Limitation Availability
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