MAKO LWIR HYPERSPECTRAL SENSOR DATA AS A TOOL FOR IDENTIFYING TECTONIC DISPLACEMENT, MINERALIZATION AND ALTERATION: EXAMPLES FROM THE EASTERN CALIFORNIA SHEAR ZONE

2016 ◽  
Author(s):  
Janet C. Harvey ◽  
◽  
Joann Stock ◽  
Kerry Buckland ◽  
Paul M. Adams
2016 ◽  
Author(s):  
Paul Wetmore ◽  
◽  
Lewis A. Owen ◽  
Timothy H. Dixon ◽  
Surui Xie ◽  
...  

Author(s):  
Hiroshi P. SATO ◽  
Mamoru KOARAI ◽  
Satoshi MIYASAKA ◽  
Hajime MAKITA ◽  
Hiroshi YAGI

Author(s):  
Naoko KOSAKA ◽  
Yohei MINEKAWA ◽  
Kuniaki UTO ◽  
Yukio KOSUGI ◽  
Kunio ODA ◽  
...  

2019 ◽  
Vol 521 ◽  
pp. 37-45 ◽  
Author(s):  
Perach Nuriel ◽  
David M. Miller ◽  
Kevin M. Schmidt ◽  
Matthew A. Coble ◽  
Kate Maher

2020 ◽  
Vol 11 (1) ◽  
Author(s):  
Kejie Chen ◽  
Jean-Philippe Avouac ◽  
Saif Aati ◽  
Chris Milliner ◽  
Fu Zheng ◽  
...  

AbstractOn July 4 2019, a Mw 6.5 earthquake, followed 34 h later by a Mw 7.1 event, struck Searles Valley, California. These events are part of a long-lived cluster of historical earthquakes along the Eastern California Shear Zone (ECSZ) which started in 1872 and are associated with temporarily elevated strain rates. We find that the Mw 6.5 event initiated on a right-lateral NW striking fault and then ruptured a left-lateral fault to the surface. This event triggered right-lateral slip during the Mw 7.1 earthquake. It started as a bilateral, crack-like rupture on a segment brought closer to failure by the Mw 6.5 event. The rupture evolved to pulse-like as it propagated at a relatively slow velocity (2 km/s) along a segment that was unloaded by the Mw 6.5 event. It stopped abruptly at the Coso volcanic area and at the Garlock Fault and brought some neighbouring faults closer to failure.


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