Section 4.2 “Geomechanics and scientific drilling”, Helmholtz Centre Potsdam, GFZ German Research Centre for Geosciences, Potsdam, Germany
Institute of Geological Sciences, Free University of Berlin, Berlin, Germany
Viewed
Since the preprint corresponding to this journal article was posted outside of Copernicus Publications, the preprint-related metrics are limited to HTML views.
Total article views: 1,520 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
Supplement
BibTeX
EndNote
1,196
267
57
1,520
55
82
117
HTML: 1,196
PDF: 267
XML: 57
Total: 1,520
Supplement: 55
BibTeX: 82
EndNote: 117
Views and downloads (calculated since 01 Jun 2023)
Cumulative views and downloads
(calculated since 01 Jun 2023)
Total article views: 1,366 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
Supplement
BibTeX
EndNote
1,042
267
57
1,366
55
78
113
HTML: 1,042
PDF: 267
XML: 57
Total: 1,366
Supplement: 55
BibTeX: 78
EndNote: 113
Views and downloads (calculated since 25 Oct 2023)
Cumulative views and downloads
(calculated since 25 Oct 2023)
Total article views: 154 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
BibTeX
EndNote
154
0
0
154
4
4
HTML: 154
PDF: 0
XML: 0
Total: 154
BibTeX: 4
EndNote: 4
Views and downloads (calculated since 01 Jun 2023)
Cumulative views and downloads
(calculated since 01 Jun 2023)
Viewed (geographical distribution)
Since the preprint corresponding to this journal article was posted outside of Copernicus Publications, the preprint-related metrics are limited to HTML views.
Total article views: 1,520 (including HTML, PDF, and XML)
Thereof 1,476 with geography defined
and 44 with unknown origin.
Total article views: 1,366 (including HTML, PDF, and XML)
Thereof 1,319 with geography defined
and 47 with unknown origin.
Total article views: 154 (including HTML, PDF, and XML)
Thereof 154 with geography defined
and 0 with unknown origin.
We analyze the 2022 MW 6.0 Gölyaka sequence. A high-resolution seismicity catalog revealed no spatiotemporal localization and lack of immediate foreshocks. Aftershock distribution suggests the activation of the Karadere and Düzce faults. The preferential energy propagation suggests that the mainshock propagated eastwards, which is in agreement with predictions from models, where the velocity in the two sides of the fault is different.
We analyze the 2022 MW 6.0 Gölyaka sequence. A high-resolution seismicity catalog revealed no...
