Zobrazeno 1 - 10
of 231
pro vyhledávání: '"Lut Block"'
Publikováno v:
پترولوژی, Vol 14, Iss 3, Pp 91-118 (2023)
The magmatic activities of Lut block started from the middle of Jurassic (165-162 Ma) with the intrusion of Kalate Ahani, Shahkoh and Sorkh kooh intrusive masses and reached its peak in the Tertiary. Tertiary volcanic and semi-volcanic rocks cover mo
Externí odkaz:
https://doaj.org/article/72e923b8894b4554ac54d3ab864bbafb
Publikováno v:
Geosciences, Vol 14, Iss 8, p 219 (2024)
This review synthesizes existing research to elucidate the factors driving the distinct tectonic behaviors in the western and eastern Makran subduction zone, focusing on seismic activity, uplift rate, convergence rate, coupling, and subduction angle.
Externí odkaz:
https://doaj.org/article/f8609227d7a24f66937417f982e74a30
Publikováno v:
Journal of Economic Geology, Vol 15, Iss 3, Pp 1-24 (2023)
Balazard prospecting area is located in eastern Iran, about 120 km south-west of Nehbandan in the Central part of Lut Block. This area consists of exposed Eocene volcanic rocks, intruded by several diorite and monzodiorite dykes and stocks. These int
Externí odkaz:
https://doaj.org/article/506a2d68dc404861ab2c3cc4cb30abdf
Autor:
Ebadolah Toulabi Nejad, Ahmad Ahamadi Khalaji, Mohammad Ebrahimi, Habib Biabangard, Rasoul Esmaeili
Publikováno v:
پترولوژی, Vol 14, Iss 2, Pp 1-30 (2023)
The Zorrati granitoid (ZG) pluton exposed on the eastern edge of the Lut block trending north-south. The Lut block surrounded in the north by the Darone fault, in the south by the Jazmurian fault and in the east and the west by Nahbandan and Naiband
Externí odkaz:
https://doaj.org/article/a0647eeb94ab4aac830d458d0224aa18
Publikováno v:
پترولوژی, Vol 13, Iss 3, Pp 85-104 (2022)
IntroductionGranites are among the most abundant rocks associated with orogenic regions that have a wide range of compositions (Atherton and Tarney, 1979; Pitcher, 1993). Among the main environments related to orogeny are continental arcs and subduct
Externí odkaz:
https://doaj.org/article/6769e241dbd9428babac288f9de07e13
Publikováno v:
پترولوژی, Vol 12, Iss 1, Pp 41-62 (2021)
Agates of the Ferdows area (north of Lut Block) occurred in open space and cracks filling form in the Paleogene volcanic rocks. These rocks are found as red, smoky, blue, violet, green, and colorless and as a vein, mosaic, geode, banded, stellar, cau
Externí odkaz:
https://doaj.org/article/7a8a918d67034b00a1f9acc7ba441e70
Autor:
Abadullah Toulabi Nejad, Ahmad Ahamadi Khalaji, Mohammad Ebrahimi, Habib Biabangard, Rasoul Esmaeili
Publikováno v:
پترولوژی, Vol 12, Iss 1, Pp 63-92 (2021)
The Malek Chah Rouii granitoid pluton is exposed within the Deh-Salm metamorphic complex in the eastern margin of the Lut zone. The studied granitoid with peraluminous and calc-alkaline nature is composed of tonalite, granodiorite, and granite (monzo
Externí odkaz:
https://doaj.org/article/211149586ff94a07808813ff974bbbdb
Publikováno v:
Journal of Asian Earth Sciences: X, Vol 7, Iss , Pp 100081- (2022)
Iranian porphyry copper deposits (PCDs), resulted from the evolution of Neo–Tethys Ocean during the Mesozoic and Cenozoic, dominantly distributed in the five main tectono-magmatic belts that meanwhile the Kerman Porphyry Copper Belt (KPCB) is the m
Externí odkaz:
https://doaj.org/article/26db40f5f1c544ec8ccdfbf76355463f
Publikováno v:
Journal of Economic Geology, Vol 12, Iss 3, Pp 377-397 (2020)
Introduction The study area is located in the Khorasan Razavi Province, NW of Gonabad between 58° 33˝- 58 ° 38˝ to the east and 25° 34˝ - 25° 38˝ to the north. Geotectonically, the area is located in the northern part of the Lut Block. The
Externí odkaz:
https://doaj.org/article/a20ce9cd4b0d4aae95c53988fde7a1f4
Publikováno v:
پترولوژی, Vol 11, Iss 2, Pp 19-36 (2020)
Hanar intrusion located in 155 km South of Birjand in the east of Lut block and compositionally consist of tonalite, granodiorite, quartz-diorite and diorite that intruded as stock and dikes in volcanic sequence (basic to intermediate) outcropped in
Externí odkaz:
https://doaj.org/article/efdefd117d9149e1a59f51ecc7fb4c04