3-D magnetotelluric imaging of the Phayao Fault Zone, Northern Thailand: Evidence for saline fluid in the source region of the 2014 Chiang Rai earthquake. (1st October 2017)

• Record Type: Journal Article
• Authors: Boonchaisuk, Songkhun; Noisagool, Sutthipong; Amatyakul, Puwis; Rung-Arunwan, Tawat; Vachiratienchai, Chatchai; Siripunvaraporn, Weerachai
• Is Part Of: Journal of Asian earth sciences. Volume 147(2017)
• Page Start: 210
• Page End: 221
• Publication Date: 2017-10-01
• Subjects: Magnetotelluric -- Northern Thailand -- Earthquake -- Fluid -- Phayao Fault Zone; Earth sciences -- Asia -- Periodicals; Sciences de la terre -- Asie -- Périodiques; Earth sciences; Asia; Periodicals; 555.05
• DOI: 10.1016/j.jseaes.2017.07.034
• Languages: English
• ISSNs: 1367-9120

Abstract

Graphical abstract: Highlights: The Phayao Fault Zone (PFZ) in Thailand is imaged via a 3-D magnetotelluric survey. The shallow 3-D resistivity structure matches well with the surface geology. A deep conductor related to the saline fluid is observed beneath the PFZ. A high fault plane instability and saline fluid govern the slip of the PFZ. Abstract: Seismicity in Thailand had been relatively low for decades prior to the Mw 6.5 earthquake of 5 May 2014 which came as a surprise and was followed by thousands of aftershocks. Most of the epicenters were located in the transition region between the Mae Lao Segment (MLS) and the Pan Segment (PS) of the Phayao Fault Zone (PFZ). We conducted a 3-D magnetotelluric (MT) survey (31 sites) to image the deep PFZ structure. The shallow 3-D resistivity structure matches very well with the surface geology, while the deeper structures disclose many interesting resistive and conductive anomalies. However, the most interesting feature of this study is the large conductive anomaly (ML) located at a depth of 4 km to the mid-crust beneath the MLS near the seismogenic zone. Our current hypothesis is that the ML conductor has a highly interconnected aqueous fluid content and also plays crucial role in the earthquake sequence of the 5 May 2014 event. As our previous seismic waveform study revealed that the MLS has a relatively high fault plane instability, the fluid within the fractured fault would further reduce the fault strength. The accumulated pre-existing tectonic stress from the north can therefore overcome the maximum frictional strength of the MLS, and hence cause it to slip and produce the main shock. With the local structural heterogeneities and fluid in the fractured fault zones, the aftershocks then occurred on both the PS and MLS. This is in contrast to the Mae Chan Fault Zone (MCFZ) in the north which many scientists expected to generate a larger magnitude earthquake than any other faults. Since instrumental record, it has only generated a few Mw 4 earthquakes. Some of our MT stations were located within the MCFZ. However, there is no deep conductor as the conductor lies beneath the MLS. A lack of interconnected fluid within the deep fault beneath the MCFZ might be one of the reasons for the lower seismic activity from the MCFZ. Other geophysical methods, such as seismic tomography, are necessary in order to confirm the presence of the fluid beneath the MLS and also the lack of a deep conductor beneath the MCFZ.