FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W3047702983> ?p ?o ?g. }

• W3047702983 startingPage "7706" @default.
• W3047702983 abstract "In order to improve our understanding of hazardous ground failures, caving processes, and collapses of large natural or man-made underground cavities, we studied microseismicity induced by the development and collapse of a salt solution mining cavity with a diameter of~ 200 m at Cerville-Buissoncourt in Lorraine, France. Microseismicity was recorded as part of a large geophysical, multi-parameter monitoring research project (GISOS) by a local, high resolution, triggered 40 Hz geophone monitoring system consisting of five one-component and four three-component borehole stations located around and in the center of the cavity. The recorded microseismic events are very numerous ( ~ 50.000 recorded event files) where the major portion ( ~ 80 %) appear in unusual swarming sequences constituted by complex clusters of superimposed microseismic events. Body wave phase based routine tools for microseismic event detection and localization face strung limitations in the treatment of these signals. Th overcome these shortcomings, we developed two probabilistic methods being able to assess the spatia-temporal charactetistics in a semi-automatic manner. The first localization approach uses simple signal amplitude estimates on different frequency bands, and an attenuation model to constrain hypocenter source location. The second approach was designed to identify siguificantly polarized P wave energies and the associated polarization angles. Both approaches and its probabilistic conjunction were applied to the data of a two months lasting microseismic crisis occurring one year before the final collapse that was related to caving processes leading to a maximal growth of ~ 50 m of the cavity roof. The obtained epicenter locations show systematic spatio-temporal migration trends observed for different time scales. During three phases of major swarming activity, epicenter migration trends appear in the order of several seconds to minutes, are spatially constrained, and show partially a reversal and cyclic spatio-temporal behavior. Similar epicenter migration trends are observed in the order of hours, and days from the spatio-temporal distribution of epicenter clusters in the cavity zone. From these observations and other geophysical parameters we conclude that microseismicity mainly represents detachment cracking at the cavity roof which is in a critical state of stress. Furthermore, we assume that the systematic epicenter migration trends represent chain reaction failures initiated by partial fracturing and subsequent stress redistribution processes. These preliminary results give first evidence that local microseismic monitoring can be a very powerful tool in order to survey and study hazardous caving processes. In future work, these hypotheses will be further tested and specified by detailed analysis of the spectru-energetic mircoseismic signal characteristics and comparison to local geodetic deformation data." @default.
• W3047702983 created "2020-08-13" @default.
• W3047702983 creator A5035851762 @default.
• W3047702983 creator A5040857813 @default.
• W3047702983 creator A5050981867 @default.
• W3047702983 creator A5064159185 @default.
• W3047702983 creator A5085739499 @default.
• W3047702983 creator A5008367136 @default.
• W3047702983 date "2014-04-27" @default.
• W3047702983 modified "2023-10-01" @default.
• W3047702983 title "Insights to caving processes from localization of microseismic swarms induced by salt solution mining" @default.
• W3047702983 hasPublicationYear "2014" @default.
• W3047702983 type Work @default.
• W3047702983 sameAs 3047702983 @default.
• W3047702983 citedByCount "0" @default.
• W3047702983 crossrefType "journal-article" @default.
• W3047702983 hasAuthorship W3047702983A5008367136 @default.
• W3047702983 hasAuthorship W3047702983A5035851762 @default.
• W3047702983 hasAuthorship W3047702983A5040857813 @default.
• W3047702983 hasAuthorship W3047702983A5050981867 @default.
• W3047702983 hasAuthorship W3047702983A5064159185 @default.
• W3047702983 hasAuthorship W3047702983A5085739499 @default.
• W3047702983 hasConcept C111357193 @default.
• W3047702983 hasConcept C121332964 @default.
• W3047702983 hasConcept C127313418 @default.
• W3047702983 hasConcept C150560799 @default.
• W3047702983 hasConcept C165205528 @default.
• W3047702983 hasConcept C180205008 @default.
• W3047702983 hasConcept C187320778 @default.
• W3047702983 hasConcept C54187759 @default.
• W3047702983 hasConcept C62520636 @default.
• W3047702983 hasConcept C7266685 @default.
• W3047702983 hasConcept C83176761 @default.
• W3047702983 hasConceptScore W3047702983C111357193 @default.
• W3047702983 hasConceptScore W3047702983C121332964 @default.
• W3047702983 hasConceptScore W3047702983C127313418 @default.
• W3047702983 hasConceptScore W3047702983C150560799 @default.
• W3047702983 hasConceptScore W3047702983C165205528 @default.
• W3047702983 hasConceptScore W3047702983C180205008 @default.
• W3047702983 hasConceptScore W3047702983C187320778 @default.
• W3047702983 hasConceptScore W3047702983C54187759 @default.
• W3047702983 hasConceptScore W3047702983C62520636 @default.
• W3047702983 hasConceptScore W3047702983C7266685 @default.
• W3047702983 hasConceptScore W3047702983C83176761 @default.
• W3047702983 hasLocation W30477029831 @default.
• W3047702983 hasOpenAccess W3047702983 @default.
• W3047702983 hasPrimaryLocation W30477029831 @default.
• W3047702983 hasRelatedWork W1599442787 @default.
• W3047702983 hasRelatedWork W1998056239 @default.
• W3047702983 hasRelatedWork W2052967571 @default.
• W3047702983 hasRelatedWork W2183362436 @default.
• W3047702983 hasRelatedWork W2184867120 @default.
• W3047702983 hasRelatedWork W2201996295 @default.
• W3047702983 hasRelatedWork W22547816 @default.
• W3047702983 hasRelatedWork W2257432973 @default.
• W3047702983 hasRelatedWork W2323316029 @default.
• W3047702983 hasRelatedWork W2328143771 @default.
• W3047702983 hasRelatedWork W2365313582 @default.
• W3047702983 hasRelatedWork W2371697029 @default.
• W3047702983 hasRelatedWork W2388154696 @default.
• W3047702983 hasRelatedWork W2512071772 @default.
• W3047702983 hasRelatedWork W2624292530 @default.
• W3047702983 hasRelatedWork W2755906005 @default.
• W3047702983 hasRelatedWork W2806043569 @default.
• W3047702983 hasRelatedWork W2884702029 @default.
• W3047702983 hasRelatedWork W2942785250 @default.
• W3047702983 hasRelatedWork W2182958429 @default.
• W3047702983 hasVolume "16" @default.
• W3047702983 isParatext "false" @default.
• W3047702983 isRetracted "false" @default.
• W3047702983 magId "3047702983" @default.
• W3047702983 workType "article" @default.