Sort by
Items per page

Send to

Choose Destination

Search results

Items: 14


The spatial footprint of injection wells in a global compilation of induced earthquake sequences.

Goebel THW, Brodsky EE.

Science. 2018 Aug 31;361(6405):899-904. doi: 10.1126/science.aat5449.


Systematic deficiency of aftershocks in areas of high coseismic slip for large subduction zone earthquakes.

Wetzler N, Lay T, Brodsky EE, Kanamori H.

Sci Adv. 2018 Feb 14;4(2):eaao3225. doi: 10.1126/sciadv.aao3225. eCollection 2018 Feb.


Granular temperature measured experimentally in a shear flow by acoustic energy.

Taylor S, Brodsky EE.

Phys Rev E. 2017 Sep;96(3-1):032913. doi: 10.1103/PhysRevE.96.032913. Epub 2017 Sep 25.


Comment on "How will induced seismicity in Oklahoma respond to decreased saltwater injection rates?" by C. Langenbruch and M. D. Zoback.

Goebel THW, Walter JI, Murray K, Brodsky EE.

Sci Adv. 2017 Aug 9;3(8):e1700441. doi: 10.1126/sciadv.1700441. eCollection 2017 Aug.


Geophysics. Recognizing foreshocks from the 1 April 2014 Chile earthquake.

Brodsky EE, Lay T.

Science. 2014 May 16;344(6185):700-2. doi: 10.1126/science.1255202. No abstract available.


Low coseismic friction on the Tohoku-Oki fault determined from temperature measurements.

Fulton PM, Brodsky EE, Kano Y, Mori J, Chester F, Ishikawa T, Harris RN, Lin W, Eguchi N, Toczko S; Expedition 343, 343T, and KR13-08 Scientists.

Science. 2013 Dec 6;342(6163):1214-7. doi: 10.1126/science.1243641.


Low coseismic shear stress on the Tohoku-Oki megathrust determined from laboratory experiments.

Ujiie K, Tanaka H, Saito T, Tsutsumi A, Mori JJ, Kameda J, Brodsky EE, Chester FM, Eguchi N, Toczko S; Expedition 343 and 343T Scientists.

Science. 2013 Dec 6;342(6163):1211-4. doi: 10.1126/science.1243485.


Structure and composition of the plate-boundary slip zone for the 2011 Tohoku-Oki earthquake.

Chester FM, Rowe C, Ujiie K, Kirkpatrick J, Regalla C, Remitti F, Moore JC, Toy V, Wolfson-Schwehr M, Bose S, Kameda J, Mori JJ, Brodsky EE, Eguchi N, Toczko S; Expedition 343 and 343T Scientists.

Science. 2013 Dec 6;342(6163):1208-11. doi: 10.1126/science.1243719.


Anthropogenic seismicity rates and operational parameters at the Salton Sea Geothermal Field.

Brodsky EE, Lajoie LJ.

Science. 2013 Aug 2;341(6145):543-6. doi: 10.1126/science.1239213. Epub 2013 Jul 11. Erratum in: Science. 2013 Dec 20;342(6165):1446.


Continuous permeability measurements record healing inside the Wenchuan earthquake fault zone.

Xue L, Li HB, Brodsky EE, Xu ZQ, Kano Y, Wang H, Mori JJ, Si JL, Pei JL, Zhang W, Yang G, Sun ZM, Huang Y.

Science. 2013 Jun 28;340(6140):1555-9. doi: 10.1126/science.1237237.


Stress state in the largest displacement area of the 2011 Tohoku-Oki earthquake.

Lin W, Conin M, Moore JC, Chester FM, Nakamura Y, Mori JJ, Anderson L, Brodsky EE, Eguchi N; Expedition 343 Scientists.

Science. 2013 Feb 8;339(6120):687-90. doi: 10.1126/science.1229379.


Isotropic events observed with a borehole array in the Chelungpu fault zone, Taiwan.

Ma KF, Lin YY, Lee SJ, Mori J, Brodsky EE.

Science. 2012 Jul 27;337(6093):459-63. doi: 10.1126/science.1222119.


Seismic waves increase permeability.

Elkhoury JE, Brodsky EE, Agnew DC.

Nature. 2006 Jun 29;441(7097):1135-8.


Decay of aftershock density with distance indicates triggering by dynamic stress.

Felzer KR, Brodsky EE.

Nature. 2006 Jun 8;441(7094):735-8.


Supplemental Content

Loading ...
Support Center