ALBERT

All Library Books, journals and Electronic Records Telegrafenberg

feed icon rss

Your email was sent successfully. Check your inbox.

An error occurred while sending the email. Please try again.

Proceed reservation?

Export
Filter
  • Other Sources  (2)
  • 2015-2019  (1)
  • 2010-2014  (1)
  • 1955-1959
Collection
Language
Years
Year
  • 1
    Publication Date: 2023-03-29
    Description: Herdflächenlösungen stellen Bruchflächen von Scherbrüchen geometrisch im Raum dar und werden aus den Polaritäten von Erdbebenwellen bestimmt. Einige der induzierten Mikroerdbeben im Bereich Landau und Insheim in der Südpfalz, die sich seit 2006 ereignen, wurden mit ausreichendem Signal-Rausch-Verhältnis an genügend vielen Messstationen beobachtet, um Herdflächenlösungen berechnen zu können. Diese Lösungen können unter Einbeziehung von Relativlokalisierungen und bekannten tektonischen Strukturen als bevorzugt nordnordwest-südsüdost (NNWSSo) streichende Scherbrüche interpretiert werden. Die Scherbrüche haben meist einen Abschiebungsmechanismus mit einer dextralen Blattverschiebungskomponente, deren Anteil variiert. Die untersuchten Erdbeben werden durch Fluidinjektion erklärt, welche die Scherfestigkeit präexistenter Strukturelemente der Rheingrabenbildung reduziert und diese alten Bruchflächen reaktiviert haben.
    Description: Abstract: In the region of Landau and Insheim, Central upper Rhine Graben, SW Germany, micro-earthquakes occur since spring 2006 due to fluid injection in the uppermost crust. These events provide important information on the structures and state of stress at depth. Here we determine fault plane solutions of the micro-earthquakes in order to understand the rupture mechanisms and stress relations at depths. Together with the relative locations of the hypocentres a prevailing NNW-SSE striking normal faulting regime is found which has a variable minor dextral strike-slip component. This result can be well explained with existing NNW-SSE striking faults which were formed during the opening of the upper Rhine Graben. These faults are reac - tivated by the fluid injection which most probably reduces the normal stress on the faults due to the fluid pressure at depth.
    Description: 1. Hintergrund 2. untersuchungsgebiet 3. Methode 4. Datenaufbereitung und Datenanalyse 5. Ergebnisse 6. Synthetische Modellierung 7. Interpretation Schriften
    Description: research
    Keywords: ddc:551.22 ; Erdbeben ; Pfalz ; Oberrheingraben
    Language: German
    Type: doc-type:article , publishedVersion
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 2
    Publication Date: 2020-01-02
    Description: Evidence for gas-hydrate occurrence in the Western Black Sea is found from seismic measurements revealing bottom-simulating reflectors (BSRs) of varying distinctness. From an ocean-bottom seismic data set low-resolution traveltime-tomography models of P-wave velocity vP are constructed. They serve as input for acoustic full-waveform inversion (FWI) which we apply to derive high-resolution parameter models aiding the interpretation of the seismic data for potential hydrate and gas deposits. Synthetic tests show the applicabilityof the FWI approach to robustly reconstruct vP models with a typical hydrate and gas signature. Models of S-wave velocity vS containing a hydrate signature can only be reconstructed when the parameter distribution of vS is already well known. When we add noise to the modeled data to simulate field data conditions, it prevents the reconstruction of vS completely, justifying the application of an acoustic approach. We invert for vP models from field-data of two parallel profiles of 14 km length with a distance of 1 km. Results showa characteristic velocity trend for hydrate and gas occurrence at BSR depth in the first of the analyzed profiles. We find no indications for gas accumulations below the BSR on the second profile and only weak indications for hydrate. These differences in vP signature are consistent with reflectivity behavior of the migrated seismic streamer data of both profiles where a zone of high reflectivity amplitudes is coincident with the potential gas zone derived from the FWI result. Calculating saturation estimates for the potential hydrate and gas zones yields values of up to 30% and 1.2%, respectively.
    Type: Article , PeerReviewed
    Format: text
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
Close ⊗
This website uses cookies and the analysis tool Matomo. More information can be found here...