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Most benchmarks located around Shin-dake crater showed crater-centered radial horizontal displacements.
Meanwhile, small displacements were detected at the benchmarks located at the foot of Kuchinoerabu-jima.
Most benchmarks located around the Shin-dake crater showed crater-centered radial horizontal displacements.
On the other hand, small displacements with less than 2 cm were detected at the benchmarks located at the foot of Kuchinoerabu-jima.
The results obtained from the comparison of 2003 and 2005 surveys indicate: (i) a lack of significant displacement (especially shortening) in the Serrania del Interior (Neogene cordillera overthrusted above the Guyana craton), (ii) an eastward displacement (relative to fixed south America plate) up to 22 mm/year of benchmarks located north of the El Pilar Fault.
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Mostly located inside of the reservoir boundary and there is one absolute gravity benchmark located outside of reservoir area.
The input data for all used benchmarks are located in the internal data memory.
In addition, AXAY benchmarks are located in Shahriar plain, starting from south of Karaj.
Large negative anomaly typically occured at the gravity benchmarks that located near to medium or high production wells.
HSHT, HQHS and HTHX benchmarks are located in southwestern and southern area of Tehran city and are representative of subsidence in the city.
The corresponding areas for the images captured by the cameras to be benchmarked are located using area descriptors.
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