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The range occurs at a major stepover zone along the Tonhil dextral strike-slip fault within a wider region dominated by late Cenozoic transpressional deformation.
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To the southeast, Profile b crosses through the stepover zone between segments of the Mae Chan fault from stations 1650 2400.
A restraining stepover zone (in compression) does not indicate a zone of open extensional fractures needed to explain the upward flow of geothermal water.
The apparent 36°SE dip between those stations also occurs on profile a and may be a tilted structure within the stepover zone.
The zone from station 2000 to 2400 is within the stepover zone of the Mae Chan fault, and we are uncertain how the MT imaging resolves this zone, except that crystalline rock contact (blue color) appears to dip more steeply from 500 to 1200 m depth over this distance.
The segments are 3 5 km long and the stepover zones are 0.5 km wide (Fig. 4).
a Attributes and features associated with stepover zones (after Micklethwaite et al. 2010).
"Major life zone" is the European phrase for the North American biome concept.
One is that the economies of some major euro zone nations will continue to stagnate.
A major euro zone meltdown would cause severe damage around the world.
The subventricular zone (SVZ) is a major germinal zone which persists in the adult brain.
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