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Issues

ISSN 0895-0695
EISSN 1938-2057

OPINION

Seismological Research Letters March 06, 2019, Vol.90, 1071-1077. doi:10.1785/0220180368

IN MEMORIAM

Seismological Research Letters April 10, 2019, Vol.90, 1078. doi:10.1785/0220190070

ARTICLES

Seismological Research Letters April 10, 2019, Vol.90, 1079-1087. doi:10.1785/0220180319
Seismological Research Letters March 06, 2019, Vol.90, 1088-1098. doi:10.1785/0220180367
Seismological Research Letters April 03, 2019, Vol.90, 1099-1110. doi:10.1785/0220190029
Seismological Research Letters February 27, 2019, Vol.90, 1111-1120. doi:10.1785/0220180262
Seismological Research Letters March 27, 2019, Vol.90, 1121-1130. doi:10.1785/0220180268
Seismological Research Letters February 27, 2019, Vol.90, 1131-1144. doi:10.1785/0220180155
Seismological Research Letters March 27, 2019, Vol.90, 1145-1154. doi:10.1785/0220180337
Seismological Research Letters April 10, 2019, Vol.90, 1155-1167. doi:10.1785/0220190007
Seismological Research Letters April 03, 2019, Vol.90, 1168-1176. doi:10.1785/0220180244
Seismological Research Letters February 20, 2019, Vol.90, 1177-1190. doi:10.1785/0220180342
Seismological Research Letters April 10, 2019, Vol.90, 1191-1199. doi:10.1785/0220180276
Seismological Research Letters April 03, 2019, Vol.90, 1200-1208. doi:10.1785/0220180242
Seismological Research Letters April 10, 2019, Vol.90, 1209-1218. doi:10.1785/0220180349
Seismological Research Letters March 13, 2019, Vol.90, 1219-1229. doi:10.1785/0220180248
Seismological Research Letters March 27, 2019, Vol.90, 1230-1242. doi:10.1785/0220180194
Seismological Research Letters March 20, 2019, Vol.90, 1243-1257. doi:10.1785/0220180245
Seismological Research Letters April 03, 2019, Vol.90, 1258-1267. doi:10.1785/0220180265
Seismological Research Letters February 27, 2019, Vol.90, 1268-1284. doi:10.1785/0220180261
Seismological Research Letters March 27, 2019, Vol.90, 1285-1295. doi:10.1785/0220180322
Seismological Research Letters April 03, 2019, Vol.90, 1296-1307. doi:10.1785/0220180366
Seismological Research Letters April 10, 2019, Vol.90, 1308-1317. doi:10.1785/0220180257
Seismological Research Letters April 03, 2019, Vol.90, 1318-1329. doi:10.1785/0220180372
Seismological Research Letters April 10, 2019, Vol.90, 1330-1334. doi:10.1785/0220180378

RETRACTION

Seismological Research Letters March 27, 2019, Vol.90, 1335. doi:10.1785/0220190066

ELECTRONIC SEISMOLOGIST

Seismological Research Letters April 03, 2019, Vol.90, 1336-1345. doi:10.1785/0220190038

DATA MINE

Seismological Research Letters March 06, 2019, Vol.90, 1346-1354. doi:10.1785/0220180364
Seismological Research Letters April 10, 2019, Vol.90, 1355-1363. doi:10.1785/0220180402
Seismological Research Letters April 10, 2019, Vol.90, 1364-1376. doi:10.1785/0220180360

EASTERN SECTION

Seismological Research Letters March 06, 2019, Vol.90, 1377-1392. doi:10.1785/0220180163
Seismological Research Letters March 20, 2019, Vol.90, 1393-1406. doi:10.1785/0220180371
Seismological Research Letters April 10, 2019, Vol.90, 1407-1419. doi:10.1785/0220180284
Seismological Research Letters April 10, 2019, Vol.90, 1420-1435. doi:10.1785/0220180285

MEETING CALENDAR

Seismological Research Letters April 10, 2019, Vol.90, 1436. doi:10.1785/0220190077
  • Cover Image

    Cover Image

    issue cover

    Front: On 16 December 2018, an ML 5.7 earthquake struck Xingwen County, Sichuan Province, China, and on 3 January 2019, an ML 5.3 earthquake occurred 8 km to the west, resulting in extensive damage to nearby structures. Lei et al. (this issue) reports that these earthquakes are the largest and most damaging in the Changning shale gas block, where 11 ML ≥ 4.0 events (including three ML ≥ 5.0) have been observed since hydraulic fracturing (HF) began in 2014. A 3D view (top) shows a simplified geological section overlapping with relocated hypocenters for observed earthquakes. The shaded image shows the landscape and well pads in which hydraulic fracturing was performed or is ongoing. The map view (bottom) shows active HF pads and three days of pre- and aftershocks of the 16 December 2018 ML 5.7 earthquake. The shaded area shows the change of Coulomb failure stress (ΔCFS) from the ML 5.7 earthquake to receiver faults of (strike, dip, rake) = (170, 83, 12) and depth of 2 km. ZJ indicates the location of Zhoujia village, which suffered the most extensive damage.

    Back: By coincidence (and scaling) the acceleration response spectrum of the 2011 Goch (Germany) earthquake recorded at the 130 m level of the north tower of Cologne Cathedral follows the shape of this World Heritage Monument. Hinzen (this issue) describes the ground motion parameters of two similarly sized local earthquakes (ML 4.3) measured by a 40-station network with several stations with identical epicentral distances, including the five stations in the cathedral.

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