[PDF] Top 20 Tectonic Geomorphology of Iran’s Salt Structures
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Tectonic Geomorphology of Iran’s Salt Structures
... of salt, gypsum and sulfur reserves has been resulted in increase of mining activities at this ...region salt domes are distinguished as Lower Red formation and external trigger have confirmed by stretch ... See full document
12
The Growth Rate of Salt Structures
... latitudinal tectonic zonation dominated, subject to the same orientation of Paleozoic morphostructures and ...active salt tectonic genesis up to diapirs of the breached type is linked with some of ... See full document
5
Mud Diapirism on the Gorgan, North Iran
... This mud diapirs has been rise from quaternary deposits and probably mud diapirism has been started since Early Pliocene, because it has covered quaternary plain. There are not the index structures in the Gorgan ... See full document
9
The tectonic geomorphology of bedrock scarps on active normal faults in the Italian Apennines mapped using combined ground penetrating radar and terrestrial laser scanning
... GPR is a non-destructive method that interprets changes in the dielectric properties of the subsurface to determine structures and layering, which may not be identi fi able from surface observations. It operates by ... See full document
15
Lineament Tectonics and Mineralizatin in Tarom Area, North Iran
... This area has an active tectonics regim [11]-[24] in compared to the Central Iran [25]-[33], Zagros in the southern Iran [34]-[40] and salt diapiric areas in Iran [41] [42]. Also, some consept ... See full document
11
Landscapes of human evolution : models and methods of tectonic geomorphology and the reconstruction of hominin landscapes
... Maps that describe and date all the relevant active tectonic and volcanic features do not currently exist. Traditional geological maps often do not show even major active structures. For example, the active ... See full document
38
The Biggest Salt Tongue Canopy of Central Iran
... Allochthonous salt sheets [1] are being categorized as types of salt ...interesting salt structure that it has been named as the biggest salt-tongue ca- nopy of Central Iran ...Central ... See full document
6
Mud Diapirism on the Makran, Iran: Case Study on the Napag Mud Volcano
... of Iran is the main aim in this ...convergent tectonic setting between Cimmerian and oceanic part of Ara- bian plate (Figure ...Iran’s tectonic setting [4]-[6], salt diapirism [7]-[16], ... See full document
9
Salt Tectonics in the Southern Iran
... of salt plugs in southern Iran, three salt diapiric provinces have been ...hundred salt plugs which they have been formed and developed in the southern margin of ...The salt ... See full document
11
Episodic Uplift along a Quaternary Fault, A Signature of Active Deformation in Frontal Part of Karachi Arc, Southern Pakistan
... arcuate structures, collectively called as Karachi ...of tectonic geomorphology revealed that it is a capable reverse fault dipping at an angle of 60° towards west which has experienced at least ... See full document
7
Tectonic Geomorphology of Upper Cimanuk Drainage Basin, West Java, Indonesia
... Abstract— The upper Cimanuk drainage basin is an inter-mountain basin. It is surrounded by volcanoes such as Mt. Tampomas, Mt. Guntur, Mt. Dano, Mt. Kamasan, Mt. Papandayan, and Mt. Cikuray. The objective of this ... See full document
7
Tectonic Geomorphology of Atrak River, NE Iran
... basins Iran, modified from ...East Iran Mountain belt, 9: West-Central Alborz and lesser Caucasus hinterland, 10: Great Kavir-Nor- then Urmieh lake foreland basin, 11: South Great Kavirfold and thrust belt, ... See full document
9
Studying Petrology and Determining Tectonic Setting of Bidkhan Area Southeast of Iran
... The most important tectonic structures that exist are main, reverse, and relatively long quadruplet faults that have a northern-southern trend and movement. Fracture and minor faults of the strike slip with ... See full document
12
Active Tectonic Signs of Taftan Mountain (South Eastern of Iran)
... In the eastern terminal of the middle, between two Nehbandan Fault (in the west) and Harirrood Fault (in the east), in the range of an area 800 km long and 200 km wide, stacked such thick deposits flysch where contain ... See full document
12
Relative tectonic activity classification in the Kermanshah area, western Iran
... The study area is the Gharasu River basin, which is in the west of Iran. The river is located in the Zagros fold–thrust belt in the Kermanshah area (Fig. 1). The aim of this selec- tion, as a study area, is to ... See full document
15
Geochemistry and Tectonic Setting of Pleistocene Basaltic Lava Flows in the Shahre-Babak Area, NW of Kerman, Iran: Implication for the Evolution of Urumieh- Dokhtar Magmatic Assemblage
... Central Iran, the Shahre-Babak alkaline basaltic lavas should be collision related ...post-collisional tectonic setting and formed in a within-plate environment between two north-south running faults and is ... See full document
12
Proposal Sites for Spent Fuel Disposal in Egypt by Using GIS Program
... ABSTRACT: The present study uses Geographic Information System(s) (GIS) as a spatial decision support tool to select potential sites in Egypt for deep geological disposal for spent radioactive fuel. A specific ... See full document
9
Analysis and Tectonic Synthesis of the Multiscale Structures along the Shangdan Tectonic Zone in the Qinling Orogenic Belt, China
... Qin, J.F., Lai, S.C., Grapes, R., Diwu, C., Ju, Y.J., Li, Y.F., 2009. Geochemical evidence for origin of magma mixing for the Triassic monzonitic granite and its enclaves at Mishuling in the Qinling orogen (central ... See full document
295
An Investigation of Deformation Structures and Their Tectonic Significance Across the Grenville Front Tectonic Zone in the Vicinity of Sudbury, Ontario, Canada
... against Jamieson (2010)’s model. In contrast to the relatively large volume 1070-1045 Ma igneous plutons in the Central Granulite Terrane in the southwest Grenville Province, igneous emplacement during or ... See full document
357
Formation of linear planform chimneys controlled by preferential hydrocarbon leakage and anisotropic stresses in faulted fine-grained sediments, offshore Angola
... The Lower Congo Basin formed during the rifting and break- up of western Gondwana, followed by the opening of the cen- tral South Atlantic (Mascle and Phillips, 1972). Two main phases of sedimentation can be ... See full document
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