Výsledky vyhledávání - "Iaccarino S. [1]"

Kinematics and Timing Constraints in a Transpressive Tectonic Regime: The Example of the Posada-Asinara Shear Zone (NE Sardinia, Italy)

Autor: Carosi R.[1], Petroccia A.[1], Iaccarino S.[1], Simonetti M.[1], Langone A.[2], Montomoli C.[1

Publikováno v: Geosciences, Vol 10, Iss 288, p 288 (2020)
Geosciences
Volume 10
Issue 8
Geosciences (Basel) 10 (2020): 1–29. doi:10.3390/geosciences10080288
info:cnr-pdr/source/autori:Carosi R.[1], Petroccia A.[1], Iaccarino S.[1], Simonetti M.[1], Langone A.[2], Montomoli C.[1,3]/titolo:Kinematics and timing constraints in a transpressive tectonic regime: The example of the posada-asinara shear zone (NE Sardinia, Italy)/doi:10.3390%2Fgeosciences10080288/rivista:Geosciences (Basel)/anno:2020/pagina_da:1/pagina_a:29/intervallo_pagine:1–29/volume:10

Detailed geological field mapping, integrated with meso- and microstructural investigations, kinematic of the flow and finite strain analyses, combined with geochronology, are fundamental tools to obtain information on the temperature&ndash
defo

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::c01854de162f2aaa4ff7f96addfd6c7e
https://www.mdpi.com/2076-3263/10/8/288

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The Main Central Thrust zone along the Alaknanda and Dhauli Ganga valleys (Garhwal Himalaya, NW India): Insights into an inverted metamorphic sequence

Autor: Iaccarino S.[1], Montomoli C.[1, Montemagni C.[3], Massonne H.-J.[4, Langone A.[6], Jain A.K.[7], Visonà D.[8], Carosi R.[1]

Publikováno v: Lithos (Oslo. Print) 372-373 (2020): 1–20. doi:10.1016/j.lithos.2020.105669
info:cnr-pdr/source/autori:Iaccarino S.[1], Montomoli C.[1,2], Montemagni C.[3], Massonne H.-J.[4,5], Langone A.[6], Jain A.K.[7], Visonà D.[8], Carosi R.[1]/titolo:The Main Central Thrust zone along the Alaknanda and Dhauli Ganga valleys (Garhwal Himalaya, NW India): Insights into an inverted metamorphic sequence/doi:10.1016%2Fj.lithos.2020.105669/rivista:Lithos (Oslo. Print)/anno:2020/pagina_da:1/pagina_a:20/intervallo_pagine:1–20/volume:372-373

New tectono-metamorphic data along the Alaknanda-Dhauli Ganga valleys in the Garhwal Himalaya (NW India) are presented focusing on sheared rocks of the Main Central Thrust zone (MCTz), one of the first order regional structures in the Himalaya. In re

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::6d8a21f17da1667873b4ad842aac22a6
http://hdl.handle.net/10281/314324

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Timing and kinematics of flow in a transpressive dextral shear zone, Maures Massif (Southern France)

Autor: Simonetti M.[1], Carosi R.[1], Montomoli C.[1, Corsini M.[3], Petroccia A.[1], Cottle J.M.[4], Iaccarino S.[1]

Publikováno v: International journal of earth sciences (1999, Print) 109 (2020): 2261–2285. doi:10.1007/s00531-020-01898-6
info:cnr-pdr/source/autori:Simonetti M.[1], Carosi R.[1], Montomoli C.[1,2], Corsini M.[3], Petroccia A.[1], Cottle J.M.[4], Iaccarino S.[1]/titolo:Timing and kinematics of flow in a transpressive dextral shear zone, Maures Massif (Southern France)/doi:10.1007%2Fs00531-020-01898-6/rivista:International journal of earth sciences (1999, Print)/anno:2020/pagina_da:2261/pagina_a:2285/intervallo_pagine:2261–2285/volume:109

The Maures–Tanneron Massif and the Corsica–Sardinia Block are two segments of the southern European Variscan belt that separated during the Late Oligocene–Miocene due to the opening of the Western Mediterranean basin. Correlation between the tw

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::39981a22e4657a75317b3186f2f06a00
http://www.cnr.it/prodotto/i/432118

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Mapping tectono-metamorphic discontinuities in orogenic belts: implications for mid-crust exhumation in NW Himalaya

Autor: Benetti B.[1], Montomoli C.[1, Iaccarino S.[1], Langone A.[3], Carosi R.[1]

Publikováno v: Lithos (Oslo. Print) 392-393 (2021): 1–23. doi:10.1016/j.lithos.2021.106129
info:cnr-pdr/source/autori:Benetti B.[1], Montomoli C.[1,2], Iaccarino S.[1], Langone A.[3], Carosi R.[1]/titolo:Mapping tectono-metamorphic discontinuities in orogenic belts: implications for mid-crust exhumation in NW Himalaya/doi:10.1016%2Fj.lithos.2021.106129/rivista:Lithos (Oslo. Print)/anno:2021/pagina_da:1/pagina_a:23/intervallo_pagine:1–23/volume:392-393

A newly identified high-temperature shear zone, the Badrinath shear zone (BSZ), is described within the metamorphic core of the Himalayan belt along the Alaknanda valley, Garhwal Himalaya (NW India). A multidisciplinary approach comprising fieldwork,

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::91bf46be5d6e9128d0b1ad0541f01307
https://doi.org/10.1016/j.lithos.2021.106129

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Pressure-Temperature-Deformation-Time Constraints on the South Tibetan Detachment System in the Garhwal Himalaya (NW India)

Autor: Iaccarino S.[1, Montomoli C.[1, Carosi R.[2], Montemagni C.[4], Massonne H.-J.[5], Langone A.[6], Jain A. K.[7], Visonà D.[8]

Publikováno v: Tectonics (Washington, D.C.) 36 (2017): 2281–2304. doi:10.1002/2017TC004566
info:cnr-pdr/source/autori:Iaccarino S.[1,2], Montomoli C.[1,3], Carosi R.[2], Montemagni C.[4], Massonne H.-J.[5], Langone A.[6], Jain A. K.[7], Visonà D.[8]/titolo:Pressure-Temperature-Deformation-Time Constraints on the South Tibetan Detachment System in the Garhwal Himalaya (NW India)/doi:10.1002%2F2017TC004566/rivista:Tectonics (Washington, D.C.)/anno:2017/pagina_da:2281/pagina_a:2304/intervallo_pagine:2281–2304/volume:36

A peculiar feature of the Himalaya is the occurrence of a system of low-angle normal faults and shear zones, the South Tibetan Detachment System (STDS), at the mountain crests. The STDS was active during synconvergent tectonics. We describe the STDS-

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=cnr_________::b6b3ef729d2af22f982d9f90fd879549
http://www.cnr.it/prodotto/i/426565

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Pressure–temperature–time–deformation path of kyanite-bearing migmatitic paragneiss in the Kali Gandaki valley (Central Nepal): Investigation of Late Eocene–Early Oligocene melting processes

Autor: Iaccarino S.[1], Montomoli C.[1, Carosi R.[3], Massonne H.-J.[4], Langone A.[5], Visona D.[6]

Publikováno v: Lithos (Oslo. Print) 231 (2015): 103–121. doi:10.1016/j.lithos.2015.06.005
info:cnr-pdr/source/autori:Iaccarino S.[1], Montomoli C.[1,2], Carosi R.[3], Massonne H.-J.[4], Langone A.[5], Visona D.[6]/titolo:Pressure-temperature-time-deformation path of kyanite-bearing migmatitic paragneiss in the Kali Gandaki valley (Central Nepal): Investigation of Late Eocene-Early Oligocene melting processes/doi:10.1016%2Fj.lithos.2015.06.005/rivista:Lithos (Oslo. Print)/anno:2015/pagina_da:103/pagina_a:121/intervallo_pagine:103–121/volume:231

Kyanite-bearing migmatitic paragneiss of the lower Greater Himalayan Sequence (GHS) in the Kali Gandaki transect (Central Himalaya) was investigated. In spite of the intense shearing, it was still possible to obtain many fundamental information for u

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::5a70d58e3097c1025d7e1d5ad0848fa3
http://hdl.handle.net/11568/759222

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Himalaya-Karakoram-Tibet Workshop. Abstract volume

Autor: Montomoli C. [1], Iaccarino S. [1], Groppo C. [2], Mosca P. [3], Rolfo F.[1], Carosi R.[2]

Publikováno v: Peshavar: National Centre of Excellence in Geology, 2014
info:cnr-pdr/source/autori:Montomoli C. [1], Iaccarino S. [1], Groppo C. [2], Mosca P. [3], Rolfo F.[1], Carosi R.[2]/titolo:Himalaya-Karakoram-Tibet Workshop. Abstract volume./editore: /anno:2014

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=cnr_________::0eed88927854a6d351b5ff262dbcfb8a
http://www.cnr.it/prodotto/i/289228

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Tectonometamorphic discontinuities within the Greater Himalayan Sequence in Western Nepal (Central Himalaya):Insights on the exhumation of crystalline rocks

Autor: Montomoli C. [1, Iaccarino S. [1], Carosi R. [2], Langone A. [3], Visonà D. [4]

Publikováno v: Tectonophysics (Amst. Online) 608 (2013): 1349–1370. doi:10.1016/j.tecto.2013.06.006
info:cnr-pdr/source/autori:Montomoli C. [1, 5], Iaccarino S. [1], Carosi R. [2], Langone A. [3], Visonà D. [4]/titolo:Tectonometamorphic discontinuities within the Greater Himalayan Sequence in Western Nepal (Central Himalaya):Insights on the exhumation of crystalline rocks./doi:10.1016%2Fj.tecto.2013.06.006/rivista:Tectonophysics (Amst. Online)/anno:2013/pagina_da:1349/pagina_a:1370/intervallo_pagine:1349–1370/volume:608

The core of the Greater Himalayan Sequence in the Mugu-Karnali area (Western Nepal) is affected by a thick shear zone with development of nearly 4 km of mylonites (Mangri shear zone). It is a contractional shear zone showing a top-to-the-SW and WSW s

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::bbfd4e8ca24e5f2b15dd63a076d577fd
https://publications.cnr.it/doc/273470

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