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Geotectonics, 2016
The Curie point depth map of Eastern Iran was constituted from spectral analysis of the aeromagnetic data. The reduction to pole (RTP) was applied to the magnetic anomaly data. The Curie point depth values from 165 overlapping blocks, 100 × 100 km in size, have been estimated.
T. Ghasemi-Rozveh +3 more
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The Curie point depth map of Eastern Iran was constituted from spectral analysis of the aeromagnetic data. The reduction to pole (RTP) was applied to the magnetic anomaly data. The Curie point depth values from 165 overlapping blocks, 100 × 100 km in size, have been estimated.
T. Ghasemi-Rozveh +3 more
openaire +1 more source
Foraminifera biozonation and morphogroups from Nimbolook section, east margin of Lut block, Iran
Arabian Journal of Geosciences, 2016One stratigraphic section named Nimbolook succession in the northwest of Qayen city was measured and sampled. Based on identified foraminifera Berthelina intermedia assemblage zone, Rotalipora appenninica and Biticinella subbreggiensis interval zones were proposed. These biozones coincide with global biozones.
Maryam Motamedalshariati +3 more
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Moment tensor and stress inversion for an active fault system in west part of Lut-Block, Iran
2015Iran is one of the most tectonically active regions on the Alpine-Himalayan earthquake belt. Eastern Iran, nowadays, is one of the most active regions of the country. The occurrence of several destructive earthquakes during the past 50 years provides the evidence for the seismic activity in this region.
Ataei, Nina, Rezapour, Mahdi
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2013
The Dehsalm porphyritic shallow intrusives belong to the Lut Block volcanic-plutonic belt (central eastern Iran). Previous research on alteration, mineralization and hydrothermal fluids indicates that a Cu-Mo porphyry type mineralization system is related with these intrusives (Arjmandzadeh et al., 2012).
Arjmandzadeh, R. +2 more
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The Dehsalm porphyritic shallow intrusives belong to the Lut Block volcanic-plutonic belt (central eastern Iran). Previous research on alteration, mineralization and hydrothermal fluids indicates that a Cu-Mo porphyry type mineralization system is related with these intrusives (Arjmandzadeh et al., 2012).
Arjmandzadeh, R. +2 more
openaire +1 more source

