Andere Kunden interessierten sich auch für
![Accuracy of GPS Precise Point Positioning]( "Accuracy of GPS Precise Point Positioning")
Accuracy of GPS Precise Point Positioning32,99 €![Artificial Intelligence for Global Positioning System Networks]( "Artificial Intelligence for Global Positioning System Networks")
Artificial Intelligence for Global Positioning System Networks46,99 €![Early Production System (EPS) Barge Movement]( "Early Production System (EPS) Barge Movement")
Early Production System (EPS) Barge Movement16,99 €![A High-Rate Virtual Instrument of Marine Vehicle Motions for Underwater Navigation and Ocean Remote Sensing]( "A High-Rate Virtual Instrument of Marine Vehicle Motions for Underwater Navigation and Ocean Remote Sensing")
A High-Rate Virtual Instrument of Marine Vehicle Motions for Underwater Navigation and Ocean Remote Sensing74,99 €![Heat and Fluid Flow at a Crustal Scale]( "Heat and Fluid Flow at a Crustal Scale")
Heat and Fluid Flow at a Crustal Scale64,99 €![Estimation of Crustal Thickness]( "Estimation of Crustal Thickness")
Estimation of Crustal Thickness29,99 €![Determination of Crustal Strain Field in Kumaun Himalaya]( "Determination of Crustal Strain Field in Kumaun Himalaya")
Determination of Crustal Strain Field in Kumaun Himalaya32,99 €
GPS campaign mode observations (2004-2007) in the Indo-Myanmar arc region along with the available results of GPS measurements analysis from permanent sites indicate that out of predominantly northward relative motion of about 4 cm/year between India and Sunda, Indo-Myanmar arc accommodates about 2 cm/year. The motion in the Indo-Myanmar arc is predominantly dextral with sites located east of Imphal valley moving faster than those in the west. The change in velocity in eastern and western regions occurs at the boundary of locally known fault "Churachandpur Mao Thrust (CMT)". It appears that the two blocks are demarcated by CMT and this fault dips towards east and marks the boundary between India and Myanmar plate.