2019
DOI: 10.1016/j.heliyon.2019.e01232
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Structural interpretation of Mae Suai Basin, Chiang Rai Province, based on gravity data analysis and modelling

Abstract: The Mae Suai Basin, an intermountain basin in northern Thailand, became an area of interest in 2014 following the M6.1 earthquake that reactivated the ENE-WSW trending Mae Loa Fault. This fault is associated with the Cenozoic rifting. Terrestrial gravity modelling is a suitable method to visualize subsurface geometry and understand its structural control related to the recent earthquakes. Six hundred twenty-seven terrestrial gravity stations with a spacing of ∼500 m were collected; standard gravity correction … Show more

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Cited by 11 publications
(4 citation statements)
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“…Slope S2 shows a signal source at a depth less than 1000 m. Slope S3 shows the processes of data acquisition. The graphic reveals gravity signals from shallow sources or disrupted surface noise from data acquisition processes (Kanthiya et al, 2019).…”
Section: Gravity Anomaly Interpretationsmentioning
confidence: 99%
“…Slope S2 shows a signal source at a depth less than 1000 m. Slope S3 shows the processes of data acquisition. The graphic reveals gravity signals from shallow sources or disrupted surface noise from data acquisition processes (Kanthiya et al, 2019).…”
Section: Gravity Anomaly Interpretationsmentioning
confidence: 99%
“…The dashed lines highlight the aftershock lineations. The solid lines are the active faults (DMR, 2016, Kanthiya et al,2019 A relocated hypocenter of the 2014 Thailand earthquake was obtained by Pananont et al (2017) using the double-difference algorithm HypoDD (Waldhauser, 2001): it is located at 19.733°N and 99.689°E with a 5 km hypocentral depth that is between the middle of the MLF and the top of the PF (Fig. 2).…”
Section: Figurementioning
confidence: 99%
“…The dots show the relocated aftershock(Pananont et al, 2017). The line shows the active faults(DMR, 2016;Kanthiya et al, 2019).…”
mentioning
confidence: 99%
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