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User-agent: * Disallow: /inhalt Disallow: /studium Disallow: /urz |
Title | Martin |
Description | Home Home Research Publications Astronomy Martin Schoenball Research Scientist Lawrence Berkeley National Laboratory, MS 74R316C 1 Cyclotron Road Berkeley, CA, |
Keywords | N/A |
WebSite | schoenball.de |
Host IP | 81.88.35.199 |
Location | Germany |
Site | Rank |
US$426,790
Last updated: 2022-10-08 15:48:20
schoenball.de has Semrush global rank of 24,799,827. schoenball.de has an estimated worth of US$ 426,790, based on its estimated Ads revenue. schoenball.de receives approximately 49,245 unique visitors each day. Its web server is located in Germany, with IP address 81.88.35.199. According to SiteAdvisor, schoenball.de is safe to visit. |
Purchase/Sale Value | US$426,790 |
Daily Ads Revenue | US$394 |
Monthly Ads Revenue | US$11,819 |
Yearly Ads Revenue | US$141,826 |
Daily Unique Visitors | 3,283 |
Note: All traffic and earnings values are estimates. |
Host | Type | TTL | Data |
schoenball.de. | A | 180 | IP: 81.88.35.199 |
schoenball.de. | A | 180 | IP: 81.88.32.143 |
schoenball.de. | NS | 3600 | NS Record: dns2.kontent.com. |
schoenball.de. | NS | 3600 | NS Record: dns1.kontent.com. |
schoenball.de. | MX | 3600 | MX Record: 10 mx.kontent.com. |
schoenball.de. | MX | 3600 | MX Record: 20 mx2.kontent.com. |
Home Research Publications Astronomy Martin Schoenball Research Scientist Lawrence Berkeley National Laboratory, MS 74R316C 1 Cyclotron Road Berkeley, CA, 94720 schoenball@lbl.gov Profile at Berkeley Lab //--> Google Scholar ORCID > Amateur astronomy //--> > Research interests My research is focussed on seismicity, that is induced in the surroundings of geothermal exploration and production, hydrocarbon extraction or deep waste water disposal. In my work, I study the elastic, poroelastic and inelastic changes of the tectonic stress field due to forced fluid flow and seismic and aseismic deformations in reservoirs. Further interests are on the tectonic stress field, borehole stability and the time-dependent behaviors in rock mechanics from the laboratory to the fault zone scale. Continue |
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