Relevant bibliographies by topics / Volcano-tectonic

Academic literature on the topic 'Volcano-tectonic'

Author: Grafiati
Published: 10 December 2022
Last updated: 28 January 2023

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Journal articles on the topic "Volcano-tectonic"

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Nugraha, Aulia Kharisma, Sukir Maryanto, and Hetty Triastuty. "HYPOCENTER DETERMINATION AND CLUSTERING OF VOLCANO-TECTONIC EARTHQUAKES IN GEDE VOLCANO 2015." Jurnal Neutrino 9, no. 2 (April 30, 2017): 44. http://dx.doi.org/10.18860/neu.v9i2.4103.

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<p class="abstrak"><span lang="EN-US">Gede volcano is an active volcano in West Java, Indonesia. Research about determination the volcano-tectonic earthquake source positions has given results using volcano-tectonic earthquakes data from January until November 2015. Volcano-tectonic earthquakes contained deep (VT-A) have frequency (maximum amplitude) range 5 – 15 Hz. Furthermore, they contain shallow earthquake, VT-B have range 3-5 Hz and LF have range 1-3 Hz. Geiger’s Adaptive Damping (GAD) methods used for determining the hypocenter of these volcano-tectonic (VT) events. Hypocenter distribution divided into 4 clusters. Cluster I located in the crater of Gede volcano dominated by VT-B earthquakes their depth range 2 km below MSL to 2 km above MSL including the VT-B swarm. The seismic sources in cluster I indicated dominant due to the volcanic fluid or gas filled in conduit pipes. Cluster II located at the west of Gede volcano caused by Gede-Pangrango fault-line dominated by VT-A earthquakes with depths range 1.5 km below MSL to 700 m above MSL. Cluster III located in the North of Gede volcano dominated by VT-A events there caused by graben fault area with those depths range 7.5 – 1.65 km below MSL. Cluster IV located in South West of Gede volcano contained VT-A earthquakes with depth range at 10 km below MSL and VT-B earthquakes this depth 2 km below MSL. Due to magma intrusion filled into fractures of the fault in the West of Gede volcano this shallow magma filling-fractures and degassing in subsurface assumed dominates the volcano-tectonic events from January to November 2015 due to faults extends from North to South occured in the West of Gede volcano.</span></p>
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Umakoshi, K., H. Shimizu, and N. Matsuwo. "Volcano-tectonic seismicity at Unzen Volcano, Japan, 1985–1999." Journal of Volcanology and Geothermal Research 112, no. 1-4 (December 2001): 117–31. http://dx.doi.org/10.1016/s0377-0273(01)00238-4.

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Iguchi, Masato, Haruhisa Nakamichi, Kuniaki Miyamoto, Makoto Shimomura, I. Gusti Made Agung Nandaka, Agus Budi-Santoso, Sulistiyani, and Nurnaning Aisyah. "Forecast of the Pyroclastic Volume by Precursory Seismicity of Merapi Volcano." Journal of Disaster Research 14, no. 1 (February 1, 2019): 51–60. http://dx.doi.org/10.20965/jdr.2019.p0051.

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We propose a method to evaluate the potential volume of eruptive material using the seismic energy of volcanic earthquakes prior to eruptions of Merapi volcano. For this analysis, we used well-documented eruptions of Merapi volcano with pyroclastic flows (1994, 1997, 1998, 2001, 2006, and 2010) and the rates and magnitudes of volcano-tectonic A-type, volcano-tectonic B-type, and multiphase earthquakes before each of the eruptions. Using the worldwide database presented by White and McCausland [1], we derived a log-linear formula that describes the upper limit of the potential volume of erupted material estimated from the cumulative seismic energy of distal volcano-tectonic earthquakes. The relationship between the volume of pyroclastic material and the cumulative seismic energy released in 1994, 1997, 1998, 2001, 2006, and 2010 at Merapi volcano is well-approximated by the empirical formula derived from worldwide data within an order of magnitude. It is possible to expand this to other volcanic eruptions with short (< 30 years) inter-eruptive intervals. The difference in the intruded and extruded volumes between intrusions and eruptions, and the selection of the time period for the cumulative energy calculation are problems that still need to be addressed.
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Hidayati, Sri, Antonius Ratdomopurbo, Kazuhiro Ishihara, and Masato Iguchi. "Focal Mechanism of Volcano-tectonic Earthquakes at Merapi Volcano, Indonesia." Indonesian Journal of Physics 19, no. 3 (November 3, 2016): 75–82. http://dx.doi.org/10.5614/itb.ijp.2008.19.3.3.

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Merapi (2968 m), located in central Java, is one of the most active and dangerous volcanoes in Indonesia. The volcano has repeated episodes of dome growth and collapse, producing pyroclastic flows during historical time. Volcano-tectonic (VT) earthquakes have been classified into deep (VTA) and shallow one (VTB). Since August 2000, number of VT events (M=1.0-1.6) had increased, and pyroclastic flows have successively occurred from the middle of January, 2001. The focal zone vertically extends to about 4 km deep beneath the summit. VTA events are located at the depth 2.2-4.1 km and the VTB ones at the depth shallower than 1.3 km. An aseismic zone is observed around 1.3-2.2 km deep between the hypocenter zones of the two types of VT earthquakes, interpreted as shallow magma storage. Focal mechanism of VT events was estimated by using both polarity and amplitude of P-wave first motions at 4 seismic stations, assuming double couple mechanism and homogenous medium. Determined focal mechanisms for VTA events are of normal-fault types. VTA events might originate by increase in horizontal tension when magma rose up from deeper portion. Orientation of their T-axes is nearly horizontal in NEE-SWW direction which might be affected by the E-W regional tectonic stress. As for the VTB, normal fault types dominate the deep VTB zone, while at the shallow part, both reverse fault and normal fault types are originated. The pressure increases at shallow magma storage may cause generation of deep VTB events of normal fault types. As VTB events frequently originated, corresponding to increase of multiphase (MP) events which are related to growth of lava dome, shallow VTB events of reverse fault type might be generated by horizontal compression related to pressure decrease in magma conduit due to extrusion of lava and gases, and occasionally by pressure increase at the shallow part due to accumulation of magma or volcanic gases.
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González, Pablo J. "Volcano-tectonic control of Cumbre Vieja." Science 375, no. 6587 (March 25, 2022): 1348–49. http://dx.doi.org/10.1126/science.abn5148.

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Galluzzo, Danilo, Lucia Nardone, Mario La Rocca, Antonietta M. Esposito, Roberto Manzo, and Rosa Di Maio. "Statistical moments of power spectrum: a fast tool for the classification of seismic events recorded on volcanoes." Advances in Geosciences 52 (October 27, 2020): 67–74. http://dx.doi.org/10.5194/adgeo-52-67-2020.

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Abstract. Spectral analysis has been applied to almost thousand seismic events recorded at Vesuvius volcano (Naples, southern Italy) in 2018 with the aim to test a new tool for a fast event classification. We computed two spectral parameters, central frequency and shape factor, from the spectral moments of order 0, 1, and 2, for each event at seven seismic stations taking the mean among the three components of ground motion. The analyzed events consist of volcano-tectonic earthquakes, low frequency events and unclassified events (landslides, rockfall, thunders, quarry blasts, etc.). Most of them are of low magnitude, and/or low maximum signal amplitude, therefore the signal to noise ratio is very different between the low noise summit stations and the higher noise stations installed at low elevation around the volcano. The results of our analysis show that volcano-tectonic earthquakes and low frequency events are easily distinguishable through the spectral moments values, particularly at seismic stations closer to the epicenter. On the contrary, unclassified events show the spectral parameters values distributed in a broad range which overlap both the volcano-tectonic earthquakes and the low frequency events. Since the computation of spectral parameters is extremely easy and fast for a detected event, it may become an effective tool for event classification in observatory practice.
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Hall, M. L., and C. A. Wood. "Volcano-tectonic segmentation of the northern Andes." Geology 13, no. 3 (1985): 203. http://dx.doi.org/10.1130/0091-7613(1985)13<203:vsotna>2.0.co;2.

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Borgia, Andrea, and Benjamin van Wyk de Vries. "The volcano-tectonic evolution of Concepción, Nicaragua." Bulletin of Volcanology 65, no. 4 (May 2003): 248–66. http://dx.doi.org/10.1007/s00445-002-0256-8.

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Roman, Diana C., and Katharine V. Cashman. "The origin of volcano-tectonic earthquake swarms." Geology 34, no. 6 (2006): 457. http://dx.doi.org/10.1130/g22269.1.

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Hübscher, Christian, M. Ruhnau, and P. Nomikou. "Volcano-tectonic evolution of the polygenetic Kolumbo submarine volcano/Santorini (Aegean Sea)." Journal of Volcanology and Geothermal Research 291 (January 2015): 101–11. http://dx.doi.org/10.1016/j.jvolgeores.2014.12.020.

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Dissertations / Theses on the topic "Volcano-tectonic"

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Hidayati, Sri. "Study on volcano-tectonic earthquakes at Sakurajima volcano and its surroundings." 京都大学 (Kyoto University), 2007. http://hdl.handle.net/2433/136776.

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Bracamontes, Dulce Maria Vargas. "Stress models related to volcano-tectonic earthquakes." Thesis, University of Leeds, 2011. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.540585.

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Bell, Andrew Forbes. "Patterns of volcano-tectonic seismicity at basaltic volcanoes." Thesis, University College London (University of London), 2008. http://discovery.ucl.ac.uk/1444163/.

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Accelerating rates of volcano-tectonic (VT) earthquakes are a common precursor to volcanic eruptions and reflect fracture growth within the edifice. Theoretical models interpret the patterns in terms of failure of the volcanic edifice under the magmatic load and promise improved eruption forecasting. However, many eruptions at frequently active basaltic volcanoes are reported to begin with little change in the rate of VT earthquakes, apparently in conflict with edifice failure models. This thesis investigates the spatial and temporal patterns of VT earthquakes associated with eruptive and intrusive dyke injection at three of the best studied basaltic volcanoes, Kilauea and Mauna Loa (Hawaii) and Mt Etna (Sicily), in order to constrain the processes controlling the approach to eruption and test the applicability of edifice failure models. Approximately one third of dyke injection events are preceded by more than 4 weeks of exponentially accelerating rates of earthquakes. The trends are consistent with a model where deformation is controlled by the growth of independent fractures driven by increased magma pressure. Relations between acceleration parameters, such as the total number of earthquakes and characteristic timescale, provide information as to the likely timing of dyke injection. No evidence is found for short-term power-law accelerations in the rates of earthquakes thought to correspond to the linkage of fractures and observed at subduction zone volcanoes. The seismicity associated with the remaining events has characteristics indicating that flank instability is involved in triggering injection, either through the progressive reduction in the horizontal compressive stress by flank slip or through an episode of accelerated flank slip (a so-called slow earthquake). These observations suggest that: 1) an edifice failure model provides a good basis for understanding the approach to basaltic eruptions, but 2) at unstable volcanoes, modifications of the model are required to account for the influence of flank slip.
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Sadikin, Nurlia. "Volcano-tectonic Earthquakes and Magma Supply System at Guntur Volcano, with Long-term Dormant Period." 京都大学 (Kyoto University), 2008. http://hdl.handle.net/2433/124353.

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Toombs, Andrew Charles. "Volcano-tectonic deformation and lava flow subsidence modelling using InSAR data at Nyamuragira Volcano, D.R. Congo." Thesis, University of Reading, 2011. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.553002.

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The rift volcano Nyamuragira in D.R. Congo regularly produces large- volume lava flows resulting from flank fissure eruptions. The eruptions are usually fed by near-vertical dykes whose orientation and location are controlled by local and regional stress. Fissuring occasionally occurs within the summit caldera, but dyke emplacement and fissuring is usually confined to the flanks along preferential zones of weakness which radiate away from the 2 x 2.2 km caldera. Space-borne Synthetic Aperture Radar Interferometry (InSAR) was used to measure eo-eruptive and inter-eruptive surface deformation at the volcano between 1996 and 2010 (8 eruptions). The largest line-of-sight (LOS) displacement due to dyke emplacement (42 cm) was recorded during the 2002 eruption. Previously unreported displacements have been measured for the 1998, 2001 and 2004 eruptions. Numerical modelling of the 2006 and 2010 eruptive events was tried. The . orientation and size of the dykes is, however, poorly constrained, and the nature of subsurface connectivity with the caldera is not known. Both dykes were emplaced on the southern flank and are aligned with a NNW-trending fracture zone running between Nyamuragira and nearby Nyiragongo. Two methods using regression analyses on time-series data were devised to model and remove lava flow subsidence signals from interferograms. Subsidence signals> 3cm/year have been measured and are a function of time and lava thickness. Linear rate subsidence models were found to be appropriate for most lava flows. Detailed mapping of the recent lava flows of Nyamuragira has also better constrained their location and spatial extent. By stacking interferograms we obtained mean deformation maps of the volcano revealing inter-eruptive deformation: 1. Uplift within the Eastern Pit Crater and inflation of the summit prior to the 2010 eruption; 2. Post- eruptive deflation centred on the 2010 eruption site; 3. Long-period subsidence beneath the Western Crater and rifring of the caldera and 1 immediate flanks; 4. Long-period subsidence centred on the 2006 eruptive vent thought to be associated with visco-elastic relaxation of a cooling magma body; 5. Similar subsidence fields centred on the 1998 and 2002 eruptive vents; 6. Anomalous subsidence associated with the 1991-93 lava flow; 7. The existence of an apparently stable, fault-bounded, and dyke- resistant block of Precambrian crust beneath the NW flank of the volcano, probably related to the Western Border Fault.
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Gezahegn, Berne Goitom. "The Nabro Volcano : tectonic framework and seismic hazard assessment of Eritrea." Thesis, University of Bristol, 2017. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.730905.

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Bursik, Marcus Sieh Kerry E. "Late Quaternary volcano-tectonic evolution of the Mono basin, eastern California /." Diss., Pasadena, Calif. : California Institute of Technology, 1989. http://resolver.caltech.edu/CaltechETD:etd-03282006-103736.

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George, Ophelia Ann. "The Geophysical Kitchen Sink Approach to Improving our Understanding of Volcano-Tectonic Interactions." Scholar Commons, 2016. http://scholarcommons.usf.edu/etd/6504.

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A multi-prong approach was taken in this dissertation to understand volcanic processes from both a long-term and more immediate hazard perspective. In the long-term, magma sources within the crust may produce measurable surficial response and long-wavelength gravity anomalies that provide information about the extent and depth of this magma. Long-term volcanic hazard forecasting is also improved by developing as complete a record as possible of past events. In the short-term, a long-standing question has been on the casting of precursory volcanic activity in terms of future volcanic hazards. Three studies are presented in this dissertation to address these issues. Inversion of high-resolution ground magnetic data in Amargosa Valley, NV indicates that anomaly B could be generated by a buried shield volcano. This new information changes the event count in this region which in turn affects the overall volcanic hazard estimation. Through the use of Finite Element Models (FEM) an in-depth characterization of the surficial response to magma underplating is provided for the Tohoku Volcanic Arc, Japan. These models indicate that surficial uplift was dominantly driven by mid-crustal intrusions and the magnitude and wavelength of this uplift was mainly controlled by the elastic layer thickness. In Dominica, seismic data were used as weights in spatial intensity maps to generate dynamic volcanic hazard maps influenced by changes in seismicity. These maps show an increasing trend in the north that may be indicative of an increase in earthquake and volcanic hazards.
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Jones, Joshua Robert. "Investigating volcano tectonic interactions in the Natron Rift of the East African Rift System." Diss., Virginia Tech, 2021. http://hdl.handle.net/10919/103780.

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Continental rifting, like other plate tectonic processes, plays a large role in shaping the Earth's crust. Active rift zones evolve from repeated tectonic and magmatic events including volcanic activity. Through investigations of currently and previously active rifts, scientists have discovered considerable interactions between these tectonic and magmatic processes during a rift's evolution; however questions remain about these interactions especially in youthful stages of rifts. We investigate an early phase magma-rich section of the East African Rift System (EARS), named the Eastern Branch to assess volcano-tectonic interactions. The Eastern Branch of the EARS consists of volcanically rich rifts that are actively spreading the Nubian Plate, Somalian plates, and Victoria block at different evolutionary stages making it an ideal study area for volcano-tectonic interactions. Our initial investigation of active volcano-tectonic interactions centered on a rifting event that occurred between 2007-2008 in the Natron Rift, a rift segment in the southern Eastern Branch located in Northern Tanzania. This rifting event contained multiple occurrences of tectonic, magmatic, and volcanic activity in close proximity. We examine the stress transferred from these events to the Natron Fault, which is the major border fault in the area, with analytical modeling using the USGS program Coulomb 3.4. We processed Global Positioning System (GPS) data that recorded slip on the major border fault in the region in early January 2008 and test which events could generate large enough stress changes to trigger the observed slip using a previously defined threshold of 0.1 MPa. These initial models were created using simplified model parameters, such as an elastic homogeneous half-space, and find that 1) magmatically induced stress perturbations have the potential to trigger fault slip on rift border faults, 2) magmatic events have the potential to trigger strike‐slip motions on a rift border fault, and 3) the proximity of magmatic activity may affect occurrences of slip on adjacent border faults. We then further investigate volcano-tectonic interactions in the Natron Rift by testing using numerical modeling with the CIG finite element code PyLith. We systematically test how adding topography, heterogeneous materials, and various reservoir volumes to a deflating 3 km deep magma reservoir system at the active volcano Ol Doinyo Lengai can affect stress transfer to the adjacent Natron Fault. We compare eight models with variations in topography, material properties, and reservoir volumes to calculate the percent differences between the models; to test their effects on the stress change results. We find that topography plays the largest role with the effect increasing with reservoir size. Finally, we seek to improve the capability of investigating volcano-tectonic interactions in the Natron Rift at faster time- scales by improving Global Navigation Satellite System (GNSS) positioning data (latitude, longitude, and height) collection and distribution capabilities. In the final part of this work, we describe a new Python-based data broker application, GNSS2CHORDS, that can stream real-time centimeter precision displacement data distributed by UNAVCO real-time GNSS data services to an online EarthCube cybertool called CHORDS. GNSS2CHORDS is applied to the TZVOLCANO GNSS network that monitors Ol Doinyo Lengai in the Natron Rift and its interactions with the adjacent rift border fault, the Natron Fault. This new tool provides a mechanism for assessing volcano-tectonic interactions in real-time. In summary, this work provides a new avenue for understanding volcano-tectonic interactions at unprecedented, 1-second time-scales, demonstrates slip can be triggered by small stress changes from magmatic events during early phase rifting, and provides insights into the key role of volcanic topography during volcano-tectonic interactions.
Doctor of Philosophy
Investigating interactions between active volcanoes and tectonics (fault zones) is important for understanding how continental rifts grow and evolve over time. Modern researchers use geodetic data, geologic models, and computer simulations of rift processes; like volcanic eruptions and fault movement; to understand how stress in transferred and material deforms due to rift activity. We are especially interested in understanding the stress interactions when volcanic eruptions and earthquakes happen together over a short time period. Our projects apply these tools to examine a segment of the largest active continental rift zone, the Natron Rift in the East African Rift System (EARS), to understand more about the details of these volcano-tectonic interactions when continents break apart (rifting). We first present results that stress transferred to the Natron Fault associated with magmatic activity from the volcano Ol Doinyo Lengai may trigger a major fault to move. Next, we continue our investigations into volcano-tectonic interactions by seeing how volcanic properties could affect stress transferred in the Natron Rift region. We choose to initially test stress variations associated with different 1) topography surfaces, 2) material properties, and 3) reservoir volumes associated with the volcano Ol Doinyo Lengai using a more advanced computer modeling approach. This deeper investigation provides information about the individual roles these parameters play in a younger rift region. We present results that topography has the most influence on the stress transferred to the Natron Fault in our models, and that the other parameters did not play a large role in influencing the stress transferred. Finally we work to increase the ability for researchers to perform geodetic studies in the Natron Rift by providing a new method to share surface displacement data at an unprecedented 1 position a second rate (near real-time). This new method is a data broker application called GNSS2CHORDS that can stream cm precision displacement data to an online cybertool called CHORDS. With our models and data provided through open source methods this work contributes significantly to our understanding of volcano-tectonic interactions.
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Jordan, Alexandra M. "An overview of the volcano-tectonic hazards of Portland, Oregon, and an assessment of emergency preparedness." Thesis, Massachusetts Institute of Technology, 2011. http://hdl.handle.net/1721.1/114368.

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Thesis: S.B., Massachusetts Institute of Technology, Department of Earth, Atmospheric, and Planetary Sciences, 2011.
Cataloged from PDF version of thesis.
Includes bibliographical references (pages 106-119).
Portland, Oregon, lies within an active tectonic margin, which puts the city at risk to hazards from earthquakes and volcanic eruptions. The young Juan de Fuca microplate is subducting under North America, introducing not only arc magmatism into the overlying plate, but also interplate and intraplate seismicity related to the subduction zone. Large crustal earthquakes are also probable in Portland because of the oblique strike-slip Portland Hills Fault zone. These hazards create risk to Portland residents and infrastructure because of pre-existing vulnerabilities. Much of Portland's downtown area, including the government and business districts, is at risk of ground shaking infrastructure damage, liquefaction and landslides due to earthquakes. Additionally, the city is within 110 km of three active Cascadia stratovolcanoes, two of which pose hazards from tephra and lahars. Though the city is under the umbrella of four emergency response plans-city, county, state and federal-there are critical gaps in mitigation strategies, emergency exercises and community education and outreach. Portland cannot prevent earthquakes or volcanic eruptions, but the city can reduce its vulnerability to these hazards.
by Alexandra M. Jordan.
S.B.
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Books on the topic "Volcano-tectonic"

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Bray, E. A. Du. Geology, age, and tectonic setting of the Cretaceous Sliderock Mountain volcano, Montana. Washington: U.S. G.P.O., 1998.

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Carr, Wilfred James. Stratigraphic and volcano-tectonic relations of Crater Flat Tuff and some older volcanic units, Nye County, Nevada. Washington: U.S. G.P.O., 1986.

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Acocella, Valerio. Volcano-Tectonic Processes. Springer International Publishing AG, 2022.

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Acocella, Valerio. Volcano-Tectonic Processes. Springer International Publishing AG, 2021.

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Driving Force of Tectonic Plate. Cres Huang, 2015.

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Bethke, Philip M., and Richard L. Hay. Ancient Lake Creede: its volcano-tectonic setting, history of sedimentation, and relation to mineralization in the Creede mining district. Geological Society of America, 2000. http://dx.doi.org/10.1130/spe346.

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Special Paper 346: Ancient Lake Creede: its volcano-tectonic setting, history of sedimentation, and relation to mineralization in the Creede mining district. Geological Society of America, 2000. http://dx.doi.org/10.1130/0-8137-2346-9.

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Appelgate, T. Bruce. Tectonic and volcanic structures of the southern flank of Axial Volcano, Juan de Fuca Ridge: Results from a SeaMARC I sidescan sonar survey. 1988.

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Ancient Lake Creede: Its Volcano-Tectonic Setting, History of Sedimentation, and Relation to Mineralization in the Creede Mining District (Special Paper (Geological Society of America)). Geological Society of America, 2000.

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Book chapters on the topic "Volcano-tectonic"

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Acocella, Valerio. "Correction to: Calderas." In Volcano-Tectonic Processes, C1. Cham: Springer International Publishing, 2021. http://dx.doi.org/10.1007/978-3-030-65968-4_14.

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Smith, Patrick. "Volcano-Tectonic Seismicity of Soufriere Hills Volcano, Montserrat." In Encyclopedia of Earthquake Engineering, 1–14. Berlin, Heidelberg: Springer Berlin Heidelberg, 2013. http://dx.doi.org/10.1007/978-3-642-36197-5_93-1.

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Smith, Patrick. "Volcano-Tectonic Seismicity of Soufriere Hills Volcano, Montserrat." In Encyclopedia of Earthquake Engineering, 3907–19. Berlin, Heidelberg: Springer Berlin Heidelberg, 2015. http://dx.doi.org/10.1007/978-3-642-35344-4_93.

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Thurber, Clifford H., and Alice E. Gripp. "Flexure and Seismicity Beneath the South Flank of Kilauea Volcano and Tectonic Implications." In Collected Reprint Series, 4271–78. Washington, DC: American Geophysical Union, 2014. http://dx.doi.org/10.1002/9781118782064.ch14.

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Montgomery-Brown, Emily K., Michael P. Poland, and Asta Miklius. "Delicate Balance of Magmatic-Tectonic Interaction at Kīlauea Volcano, Hawai‘i, Revealed from Slow Slip Events." In Hawaiian Volcanoes, 269–88. Hoboken, NJ: John Wiley & Sons, Inc, 2015. http://dx.doi.org/10.1002/9781118872079.ch13.

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Bertrand, H. "The Mesozoic Tholeiitic Province of Northwest Africa: A Volcano-Tectonic Record of the Early Opening of Central Atlantic." In Magmatism in Extensional Structural Settings, 147–88. Berlin, Heidelberg: Springer Berlin Heidelberg, 1991. http://dx.doi.org/10.1007/978-3-642-73966-8_7.

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Folguera, A., E. Rojas Vera, L. Vélez, J. Tobal, D. Orts, M. Agusto, A. Caselli, and V. A. Ramos. "A Review of the Geology, Structural Controls, and Tectonic Setting of Copahue Volcano, Southern Volcanic Zone, Andes, Argentina." In Active Volcanoes of the World, 3–22. Berlin, Heidelberg: Springer Berlin Heidelberg, 2015. http://dx.doi.org/10.1007/978-3-662-48005-2_1.

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Aiuppa, Alessandro, Patrick Allard, Walter D'Alessandro, Salvatore Giammanco, Francesco Parello, and Mariano Valenza. "Magmatic gas leakage at Mount Etna (Sicily, Italy): Relationships with the volcano-tectonic structures, the hydrological pattern and the eruptive activity." In Geophysical Monograph Series, 129–45. Washington, D. C.: American Geophysical Union, 2004. http://dx.doi.org/10.1029/143gm09.

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Benvenuti, M., and S. Carnicelli. "The Geomorphology of the Lake Region (Main Ethiopian Rift): The Record of Paleohydrological and Paleoclimatic Events in an Active Volcano-Tectonic Setting." In World Geomorphological Landscapes, 289–305. Dordrecht: Springer Netherlands, 2015. http://dx.doi.org/10.1007/978-94-017-8026-1_17.

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Mcnutt, S. R. "Eruptions of Pavlof Volcano, Alaska, and their Possible Modulation by Ocean Load and Tectonic Stresses: Re-evaluation of the Hypothesis Based on New Data from 1984-1998." In Seismicity Patterns, their Statistical Significance and Physical Meaning, 701–12. Basel: Birkhäuser Basel, 1999. http://dx.doi.org/10.1007/978-3-0348-8677-2_23.

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Conference papers on the topic "Volcano-tectonic"

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Ry, Rexha Verdhora, and Andri Dian Nugraha. "Improve earthquake hypocenter using adaptive simulated annealing inversion in regional tectonic, volcano tectonic, and geothermal observation." In NATIONAL PHYSICS CONFERENCE 2014 (PERFIK 2014). AIP Publishing LLC, 2015. http://dx.doi.org/10.1063/1.4915012.

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Ry, Rexha V., A. Priyono, A. D. Nugraha, and A. Basuki. "Seismicity study of volcano-tectonic in and around Tangkuban Parahu active volcano in West Java region, Indonesia." In THE 5TH INTERNATIONAL SYMPOSIUM ON EARTHHAZARD AND DISASTER MITIGATION: The Annual Symposium on Earthquake and Related Geohazard Research for Disaster Risk Reduction. Author(s), 2016. http://dx.doi.org/10.1063/1.4947372.

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Venegas, Pablo, Noel Perez, Diego S. Benitez, Roman Lara-Cueva, and Mario Ruiz. "Building Machine Learning Models for Long-Period and Volcano-Tectonic Event Classification." In 2019 IEEE CHILEAN Conference on Electrical, Electronics Engineering, Information and Communication Technologies (CHILECON). IEEE, 2019. http://dx.doi.org/10.1109/chilecon47746.2019.8987505.

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Harlianti, Ulvienin, Andri Dian Nugraha, and Novianti Indrastuti. "Relocation of volcano-tectonic earthquake hypocenter at Mt. Sinabung using double difference method." In INTERNATIONAL SYMPOSIUM ON EARTH HAZARD AND DISASTER MITIGATION (ISEDM) 2016: The 6th Annual Symposium on Earthquake and Related Geohazard Research for Disaster Risk Reduction. Author(s), 2017. http://dx.doi.org/10.1063/1.4987092.

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Fais, S., and E. E. Klingelè. "Volcano-Tectonic Evolution of the Offshore Cagliari Gulf (Western Mediterranean) from Geophysical Data." In 69th EAGE Conference and Exhibition incorporating SPE EUROPEC 2007. European Association of Geoscientists & Engineers, 2007. http://dx.doi.org/10.3997/2214-4609.201401844.

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Busby, Cathy J., Alison Graettinger, and Margarita Lopez. "VOLCANO-TECTONIC EVOLUTION OF THE CENTRAL BAJA CALIFORNIA GULF MARGIN: 40AR/40AR GEOCHRONOLOGICAL CONSTRAINTS." In Joint 70th Annual Rocky Mountain GSA Section / 114th Annual Cordilleran GSA Section Meeting - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018rm-314304.

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Rubin, Kenneth H., and Robert W. Embley. "TECTONIC AND VOLCANIC INTERPLAYS IN EARTH’S LARGEST AND ONLY KNOWN ACTIVE BONINITE VOLCANO PROVINCE." In GSA Annual Meeting in Denver, Colorado, USA - 2016. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016am-286764.

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Curilem, M., M. Salman Khan, N. Becerra Yoma, C. San Martin, C. Cardona, C. Soto, F. Huenupan, L. Franco, G. Acu[ntilde]a, and M. Chaco[acute ]n. "Feature Selection for Discrimination between Volcanic and Tectonic Events of The Llaima Volcano (Chile)." In International Conference on Pattern Recognition Systems (ICPRS-16). Institution of Engineering and Technology, 2016. http://dx.doi.org/10.1049/ic.2016.0034.

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Brotopuspito, K., T. Kusmita, and H. Triastuty. "Spectra analysis for source dynamic identification of deep volcano tectonic underneath mounth Sinabung, North Sumatera." In EAGE-HAGI 1st Asia Pacific Meeting on Near Surface Geoscience and Engineering. Netherlands: EAGE Publications BV, 2018. http://dx.doi.org/10.3997/2214-4609.201800381.

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Banik, Tenley J., Calvin F. Miller, Christopher M. Fisher, Matthew A. Coble, and Jeffrey D. Vervoort. "ISOTOPIC INSIGHTS ON GENERATION OF SILICIC MAGMAS IN ICELAND: CONSTRAINTS ON MAGMATIC-TECTONIC CONTROL AT HAFNARFJALL-SKARÐSHEIÐI VOLCANO." In GSA Annual Meeting in Indianapolis, Indiana, USA - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018am-317961.

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Reports on the topic "Volcano-tectonic"

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Mark Leon Gwynn. TECTONIC VERSUS VOLCANIC ORIGIN OF THE SUMMIT DEPRESSION AT MEDICINE LAKE VOLCANO, CALIFORNIA. Office of Scientific and Technical Information (OSTI), May 2010. http://dx.doi.org/10.2172/1006213.

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Weiss, S. I., D. C. Noble, and L. T. Larson. Evaluation of mineral resource potential, caldera geology, and volcano-tectonic framework at and near Yucca Mountain. Office of Scientific and Technical Information (OSTI), September 1992. http://dx.doi.org/10.2172/227020.

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Weiss, S. I., D. C. Noble, and L. T. Larson. Evaluation of minderal resource potential, Caldera geology, and volcano-tectonic framework at and near Yucca Mountain, Task 3. Office of Scientific and Technical Information (OSTI), September 1993. http://dx.doi.org/10.2172/227026.

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Weiss, S. I., D. C. Noble, and L. T. Larson. Task 3: Evaluation of mineral resource potential, caldera geology, and volcano-tectonic framework at and near Yucca Mountain. Office of Scientific and Technical Information (OSTI), December 1994. http://dx.doi.org/10.2172/240929.

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Abebe, Tsegaye. Geological map (scale 1:200,000) of the northern Main Ethiopian Rift and its implications for the volcano-tectonic evolution of the rift. Geological Society of America, January 2005. http://dx.doi.org/10.1130/mch094.

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Wilson, A. M., and M. C. Kelman. Assessing the relative threats from Canadian volcanoes. Natural Resources Canada/CMSS/Information Management, 2021. http://dx.doi.org/10.4095/328950.

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This report presents an analysis of the threat posed by active volcanoes in Canada and outlines directives to bring Canadian volcano monitoring and research into alignment with global best practices. We analyse 28 Canadian volcanoes in terms of their relative threat to people, aviation and infrastructure. The methodology we apply to assess volcanic threat was developed by the United States Geological Survey (USGS) as part of the 2005 National Volcano Early Warning System (NVEWS). Each volcano is scored on a number of hazard and exposure factors, producing an overall threat score. The overall threat scores are then assigned to five threat categories ranging from Very Low to Very High. We adjusted the methodology slightly to better suit Canadian volcano conditions by adding an additional knowledge uncertainty score; this does not affect the threat scoring or ranking. Our threat assessment places two volcanoes into the Very High threat category (Mt. Meager and Mt. Garibaldi). Three Canadian volcanoes score in the High threat category (Mt. Cayley, Mt. Price and Mt. Edziza) and two volcanoes score in the Moderate threat category (the Nass River group and Mt. Silverthrone). We compare the ranked Canadian volcanoes to similarly scored volcanoes in the USA and assess the current levels of volcano monitoring against internationally recognised monitoring strategies. We find that even the most thoroughly-studied volcano in Canada (Mt. Meager) falls significantly short of the recommended monitoring level (Mt. Meager is currently monitored at a level commensurate with a Very Low threat edifice, according to NVEWS recommendations). All other Canadian volcanoes are unmonitored (other than falling within a regional seismic network emplaced to monitor tectonic earthquakes). Based on the relative threat and scientific uncertainty surrounding some Canadian volcanoes, we outline five strategies to improve volcano monitoring in Canada and lower the uncertainty about eruption style and frequency: installation of real-time seismic stations at all Very High and High threat volcanoes, comprehensive lithofacies studies at Mt. Garibaldi in order to reduce uncertainty surrounding the frequency and style of volcanism, hazard mapping at Mt. Garibaldi and Mt. Cayley and publication of existing hazard analyses and mapping for Mt. Meager as a comprehensive hazard map, regular satellite-based ground deformation monitoring at all Very High to Moderate threat edifices, and, finally, installation of a landslide detection and alerting system at Mt. Meager.
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Wilson, A. M., and M. C. Kelman. Assessing the relative threats from Canadian volcanoes. Natural Resources Canada/CMSS/Information Management, 2021. http://dx.doi.org/10.4095/328950.

Full text
Abstract:
This report presents an analysis of the threat posed by active volcanoes in Canada and outlines directives to bring Canadian volcano monitoring and research into alignment with global best practices. We analyse 28 Canadian volcanoes in terms of their relative threat to people, aviation and infrastructure. The methodology we apply to assess volcanic threat was developed by the United States Geological Survey (USGS) as part of the 2005 National Volcano Early Warning System (NVEWS). Each volcano is scored on a number of hazard and exposure factors, producing an overall threat score. The overall threat scores are then assigned to five threat categories ranging from Very Low to Very High. We adjusted the methodology slightly to better suit Canadian volcano conditions by adding an additional knowledge uncertainty score; this does not affect the threat scoring or ranking. Our threat assessment places two volcanoes into the Very High threat category (Mt. Meager and Mt. Garibaldi). Three Canadian volcanoes score in the High threat category (Mt. Cayley, Mt. Price and Mt. Edziza) and two volcanoes score in the Moderate threat category (the Nass River group and Mt. Silverthrone). We compare the ranked Canadian volcanoes to similarly scored volcanoes in the USA and assess the current levels of volcano monitoring against internationally recognised monitoring strategies. We find that even the most thoroughly-studied volcano in Canada (Mt. Meager) falls significantly short of the recommended monitoring level (Mt. Meager is currently monitored at a level commensurate with a Very Low threat edifice, according to NVEWS recommendations). All other Canadian volcanoes are unmonitored (other than falling within a regional seismic network emplaced to monitor tectonic earthquakes). Based on the relative threat and scientific uncertainty surrounding some Canadian volcanoes, we outline five strategies to improve volcano monitoring in Canada and lower the uncertainty about eruption style and frequency: installation of real-time seismic stations at all Very High and High threat volcanoes, comprehensive lithofacies studies at Mt. Garibaldi in order to reduce uncertainty surrounding the frequency and style of volcanism, hazard mapping at Mt. Garibaldi and Mt. Cayley and publication of existing hazard analyses and mapping for Mt. Meager as a comprehensive hazard map, regular satellite-based ground deformation monitoring at all Very High to Moderate threat edifices, and, finally, installation of a landslide detection and alerting system at Mt. Meager.
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