Geophysical monograph最新文献

{"title":"Uncertainty Assessment of Pyroclastic Density Currents at Mount Vesuvius (Italy) Simulated Through the Energy Cone Model","authors":"Pablo Tierz, L. Sandri, Antonio Costa, R. Sulpizio, L. Zaccarelli, M. A. Vito, W. Marzocchi","doi":"10.1002/9781119028116.CH9","DOIUrl":"https://doi.org/10.1002/9781119028116.CH9","url":null,"abstract":"","PeriodicalId":12539,"journal":{"name":"Geophysical monograph","volume":"1 1","pages":"125-145"},"PeriodicalIF":0.0,"publicationDate":"2016-11-19","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"77417796","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"Seismic Potential of Thrust‐Wrench Tectonic Interference between Major Active Faults Offshore SW Iberia","authors":"F. Rosas, J. Duarte, W. Schellart, R. Tomás, P. Terrinha","doi":"10.1002/9781119054146.CH9","DOIUrl":"https://doi.org/10.1002/9781119054146.CH9","url":null,"abstract":"","PeriodicalId":12539,"journal":{"name":"Geophysical monograph","volume":"37 1","pages":"193-217"},"PeriodicalIF":0.0,"publicationDate":"2016-10-18","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"79043577","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"Integrated Imaging of the Earth: Theory and Applications","authors":"M. Moorkamp, P. Lelièvre, N. Linde, Amir Khan","doi":"10.1002/9781118929063","DOIUrl":"https://doi.org/10.1002/9781118929063","url":null,"abstract":"Description: Reliable and detailed information about the Earth s subsurface is of crucial importance throughout the geosciences. Quantitative integration of all available geophysical and geological data helps to make Earth models more robust and reliable. The aim of this book is to summarize and synthesize the growing literature on combining various types of geophysical and other geoscientific data. The approaches that have been developed to date encompass joint inversion, cooperative inversion, and statistical post–inversion analysis methods, each with different benefits and assumptions.","PeriodicalId":12539,"journal":{"name":"Geophysical monograph","volume":"941 1","pages":""},"PeriodicalIF":0.0,"publicationDate":"2016-04-22","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"77561247","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"Onset of a Basaltic Explosive Eruption From Kīlauea's Summit in 2008","authors":"R. Carey, L. Swavely, D. Swanson, B. Houghton, T. Orr, T. Elias, A. J. Sutton","doi":"10.1002/9781118872079.CH19","DOIUrl":"https://doi.org/10.1002/9781118872079.CH19","url":null,"abstract":"The onset of basaltic eruption at the summit of Kīlauea volcano in 2008 is recorded in the products generated during the first three weeks of the eruption and suggests an evolution of both the physical properties of the magma and also lava lake levels and vent wall stability. Ash componentry and the microtextures of the early erupted lapilli products reveal that the magma was largely outgassed, perhaps in the preceding weeks to months. An increase in the juvenile:lithic ratio and size of ash collected from March 23 to April 3 records an increasing level of the magma within the conduit. After April 3 until the explosive eruption of April 9, a trend of decreasing juvenile:lithic ratio suggests that vent wall collapses were more frequent, possibly because lava level increased and destabilized the overhanging wall [ Orr et al . 2013]. Despite increasing lake height, the microtextural characteristics of the lapilli suggest that the outgassed end-member was still being tapped between March 26 and April 8. The April 9 rockfall triggered an explosive eruption that produced a new component in the eruption deposits not seen in the preceding weeks; microvesicular juvenile lapilli, the first evidence of an actively vesiculating magma. Two additional dense end-member pyroclast types were also erupted during the April 9 explosion, likely related to outgassed magma with longer residence times than the microvesicular magma. We link these pyroclasts to a stagnant viscous crust at the top of the magma column or to convecting, downwelling magma. Our study of ash componentry and the textures of juvenile lapilli suggests that the April 9 explosive event effectively cleared the conduit of largely outgassed magma. The degassing processes during this eruption are complex and varied: in the period of persistent degassing during March 26-April 8 small resident bubbles at shallow levels in the lava lake were coupled to the magma whereas large bubbles ascended, expanded and fragmented. During the rockfall-triggered explosion of April 9, all bubbles were coupled to the host magma on the timescale of decompression, but additional exsolution, decompression and expansion of deeper, more gas-rich resident magma likely occured [cf Carey et al. 2012]. Where external conditions play a significant role in eruption dynamics, e.g., by triggering eruptions, vesiculation and degassing dynamics can be expected to be complex.","PeriodicalId":12539,"journal":{"name":"Geophysical monograph","volume":"13 1","pages":"421-437"},"PeriodicalIF":0.0,"publicationDate":"2015-02-27","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"80200871","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"“Points Requiring Elucidation” About Hawaiian Volcanism","authors":"M. Poland","doi":"10.1002/9781118872079.CH24","DOIUrl":"https://doi.org/10.1002/9781118872079.CH24","url":null,"abstract":"","PeriodicalId":12539,"journal":{"name":"Geophysical monograph","volume":"207 1","pages":"533-562"},"PeriodicalIF":0.0,"publicationDate":"2015-02-27","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"72999090","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"Evidence for Large Compositional Ranges in Coeval Melts Erupted from Kīlauea's Summit Reservoir","authors":"R. T. Helz, D. Clague, L. Mastin, T. Rose","doi":"10.1002/9781118872079.CH7","DOIUrl":"https://doi.org/10.1002/9781118872079.CH7","url":null,"abstract":"","PeriodicalId":12539,"journal":{"name":"Geophysical monograph","volume":"78 1","pages":"125-145"},"PeriodicalIF":0.0,"publicationDate":"2015-02-27","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"88103126","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"Crustal stress and structure at Kīlauea Volcano inferred from seismic anisotropy","authors":"Jessica H. Johnson, D. Swanson, D. Roman, M. Poland, W. Thelen","doi":"10.1002/9781118872079.CH12","DOIUrl":"https://doi.org/10.1002/9781118872079.CH12","url":null,"abstract":"","PeriodicalId":12539,"journal":{"name":"Geophysical monograph","volume":"1 1","pages":"251-268"},"PeriodicalIF":0.0,"publicationDate":"2015-02-27","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"86881064","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"Are Piton de la Fournaise (La Réunion) and Kīlauea (Hawai‘i) Really “Analog Volcanoes”?","authors":"A. Peltier, M. Poland, T. Staudacher","doi":"10.1002/9781118872079.CH23","DOIUrl":"https://doi.org/10.1002/9781118872079.CH23","url":null,"abstract":"","PeriodicalId":12539,"journal":{"name":"Geophysical monograph","volume":"57 1","pages":"507-531"},"PeriodicalIF":0.0,"publicationDate":"2015-02-27","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"88687861","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"Reticulite-Producing Fountains from Ring Fractures in Kīlauea Caldera ca. 1500 CE","authors":"M. May, R. Carey, D. Swanson, B. Houghton","doi":"10.1002/9781118872079.CH16","DOIUrl":"https://doi.org/10.1002/9781118872079.CH16","url":null,"abstract":"A widely dispersed reticulite bed occurs close to the base of the Keanakīko'i tephra at Kīlauea Volcano. It can be divided into six subunits in the northern sector of the volcano; the reticulite also occurs in the southern sector, but outcrops are sparse owing to penecontemporaneous erosion and burial. Multilobate isopachs for each subunit and the total deposit suggests that multiple fountaining vents were distributed in the northern half of the caldera, possibly along ring fractures for the newly formed caldera. Isopach maps also show a sharp decline in thickness along the dispersal axis of each lobe, which could be explained by remobilization of tephra and/or inclined fountains. Despite such isopach characteristics, thinning rates calculated from the isopach data indicate that the fountains were among the most intense and powerful of all studied Kīlauea fountains. Density analysis of the pyroclasts suggests that fountaining was high (< 600 meters) yet complex, possibly due to lava ponding and re-entrainment. The calculated volume of the reticulite deposited around the caldera rim is approximately 0.2 km3, more voluminous than the deposits of the 1959 Kīlauea Iki eruption; this volume is a minimum, however, as the low density tephra is easily remobilized, and 600-m-high caldera walls probably trapped tephra within caldera, which is deeply buried today and not accounted for in the volume calculations. The duration of this eruption was most likely at least a few days to weeks, based on the calculated volume and estimated discharge rates as seen during the Kīlauea Iki 1959 eruption.","PeriodicalId":12539,"journal":{"name":"Geophysical monograph","volume":"14 1","pages":"351-367"},"PeriodicalIF":0.0,"publicationDate":"2015-02-27","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"87379546","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"Onset of Rejuvenated‐Stage Volcanism and the Formation of Līhu‘e Basin","authors":"D. Sherrod, S. Izuka, B. Cousens","doi":"10.1002/9781118872079.CH6","DOIUrl":"https://doi.org/10.1002/9781118872079.CH6","url":null,"abstract":"","PeriodicalId":12539,"journal":{"name":"Geophysical monograph","volume":"12 1","pages":"105-123"},"PeriodicalIF":0.0,"publicationDate":"2015-02-27","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"80896820","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}