Special Issue: Evolution of collisional orogens in space and time—the Alpine-Himalayan system in 4 dimensions

IF 1.8 2区 地球科学 Q3 GEOSCIENCES, MULTIDISCIPLINARY
Chiara Montomoli, Salvatore Iaccarino, Jean-Luc Epard, Paola Manzotti
{"title":"Special Issue: Evolution of collisional orogens in space and time—the Alpine-Himalayan system in 4 dimensions","authors":"Chiara Montomoli, Salvatore Iaccarino, Jean-Luc Epard, Paola Manzotti","doi":"10.1186/s00015-024-00466-3","DOIUrl":null,"url":null,"abstract":"<p>This Special Issue of the Swiss Journal of Geosciences entitled “<i>Evolution of collisional orogens in space and time: the Alpine-Himalayan system in 4 dimensions</i>”, was proposed during the joint meeting “Geosciences for a sustainable future” organized by the Società Geologica Italiana and Società Italiana di Mineralogia e Petrografia held in Turin (Italy) in September 2022.</p><p>The issue focuses on the evolution of collisional orogens through a multidisciplinary approach. As a matter of fact, continental plate collisions give rise to collisional-related orogenic belts that are some of the most spectacular and dominant features on our planet.</p><p>During collision of continental plates, considerable deformation occurs with large scale overthrusting, burial and metamorphism of continental lithosphere portions. The final anatomy and the shape of collisional belts are highly diverse, due to the interactions of several controlling factors, including the pre-collisional tectonic history, the rate and the angle of convergence, the mechanical strength and thermal state of the involved colliding plates.</p><p>The youngest collisional system on Earth is the Alpine-Himalayan belt, extending from Spain to Southeast Asia. Its general structure was first described by Emile Argand in \"La tectonique de l’Asie\". On the occasion of the centenary of Argand’s work, presented during the XIII International Geological congress in Belgium (August 10, 1922), this thematic volume aims to provide an updated view on the Alpine-Himalayan geology.</p><p>This Special Issue collects multidisciplinary contributions focusing on the Alpine-Himalayan system, dealing with the reconstruction of the tectonic architecture at different scales, integrating field mapping to microscale and describing the tectono-metamorphic evolution.</p><p>The papers included in this collection span from the Himalaya to the Western, Central and Ligurian Alps and also include a paper on the Alborz Mountains in Iran.</p><p>The publication by Robyr (2023) brings us in the Himalayan belt (Miyar Valley, North-West India) and focuses on the old history of the belt studying the pre-Himalayan metamorphism of the metamorphic core of the chain, until now strongly debated. Through phase petrology and microtectonics studies, combined with valuable field data, Robyr demonstrates the existence of a pre-Himalayan orogenic cycle.</p><p>Pantet et al. (2024), focus on the region surrounding the Zermatt area (SW Switzerland and NW Italy) where continental and oceanic units are strongly imbricated. Starting from a very detailed field mapping, they focus on the structure and stratigraphy of the Permian-Jurassic continent‑derived Faisceau Vermiculaire series and associated non-ophiolitic Upper Cretaceous calcschists (Série Rousse), both intercalated within ophiolitic units. They were able to reconstruct the architecture of the Briançonnais-Prepiemont palaeomargin before the onset of Alpine deformation and the structural evolution through polyphase deformation during Alpine Tectonics.</p><p>Dana et al. (2023), investigate the structural architecture and tectono-metamorphic evolution of Briançonnais units along the Ubaye–Maira valleys (South-Western Alps) at the French-Italian boundary. The Authors, starting from detailed geological mapping and integrating microstructural and metamorphic data, obtained with the Raman Spectroscopy of Carbonaceous Material, reconstruct the evolution of the subducted Briançonnais passive margin from the pre-rifting to the Alpine collisional stage.</p><p>Manna et al. (2023), present new geological data from the Ligurian Alps. The Authors, with the aid of structural mapping, UAV photogrammetric survey and digital outcrop modelling, report the first description of a 15 km-long NE-SW-striking transtensive fault network (referred to as <i>Horse Head Fault Zone</i>) crosscutting the metamorphic units of the area. This fault zone accommodated tens of km-scale displacements related to the Adria counterclockwise rotation after the Adria-Europe collision and the beginning of the Apennine subduction rollback.</p><p>Zanchetta et al. (2024), study the Permian Val Biandino Intrusive Suite in the central sector of the South Alpine Domain (N Italy). The Authors present new detailed petrographic, geochemical, and geochronological data of this intrusive Complex emplaced in the Variscan metamorphic basement. On the basis of their new data, they provide an updated picture of the Val Biandino Intrusive Suite, demonstrating how, despite its relatively small size, it displays a significant heterogeneity in terms of rock varieties intruded in a short time interval (ca. 5 Myrs). They conclude that the Val Biandino Intrusive Suite was likely formed through the interaction of magma generated at the mantle/crust transition and partial melting of the heterogeneous pre-Permian basement of the Southalpine Domain. These processes were linked to early Permian crustal extension and heat advection from the asthenosphere.</p><p>Rezaei et al. (2023), take us back to Asia, to the Alborz Mountains of north Iran. They investigate cumulate gabbroic rocks intruding Palaeozoic metasediments and Mesozoic sediments in the Gasht-Masuleh area. With the aid of petrographic analysis, whole-rock and mineral chemistry, as well as geochronology, the Authors were able to relate the mafic magmatism of the area to extension resulting from far-field effects linked to roll-back of the Neo-Tethys subducting slab in the mid-Cretaceous time.</p><p>Last but not least, we want to thank all the Authors who contributed to this special issue presenting their works from different sectors of the Alpine-Himalayan orogenic system. We are also very grateful to the reviewers that strongly contributed to improve the quality of the manuscripts and helped for successfully publishing this Special Issue.</p><p>Not applicable.</p><ul data-track-component=\"outbound reference\" data-track-context=\"references section\"><li><p>Dana, D., Iaccarino, S., Schmid, S. M., Petroccia, A., &amp; Michard, A. (2023). Structural and metamorphic evolution of a subducted passive margin: Insights from the Briançonnais nappes of the Western Alps (Ubaye–Maira valleys, France–Italy). <i>Swiss Journal of Geosciences,</i> <i>116</i>, 18.</p><p>Article Google Scholar </p></li><li><p>Manna, L., Perozzo, M., Menegoni, N., Tamburelli, S., Crispini, L., Federico, L., Seno, S., &amp; Maino, M. (2023). Anatomy of a km-scale fault zone controlling the Oligo-Miocene bending of the Ligurian Alps (NW Italy): Integration of field and 3D high-resolution digital outcrop model data. <i>Swiss Journal of Geosciences,</i> <i>116</i>, 15.</p><p>Article Google Scholar </p></li><li><p>Pantet, A., Epard, J.-L., &amp; Masson, H. (2024). Continent-derived metasediments (Cimes Blanches and Frilihorn) within the ophiolites around Zermatt: Relations with the Mischabel backfold and Mont Fort nappe (Pennine Alps). <i>Swiss Journal of Geosciences,</i> <i>117</i>, 10.</p><p>Article Google Scholar </p></li><li><p>Rezaei, L., Timmerman, M. J., Moazzen, M., Altenberger, U., Sláma, J., Sudo, M., Günter, C., Wilke, F. D. H., &amp; Schleicher, A. M. (2023). Mid-Cretaceous extensional magmatism in the Alborz Mountains, north Iran; geochemistry and geochronology of Gasht-Masuleh gabbros. <i>Swiss Journal of Geosciences,</i> <i>116</i>, 14.</p><p>Article CAS Google Scholar </p></li><li><p>Robyr, M. (2023). Evidence for a pre-Himalayan metamorphism in the High Himalayan Crystalline of the Miyar Valley (NW India). <i>Swiss Journal of Geosciences,</i> <i>116</i>, 17.</p><p>Article Google Scholar </p></li><li><p>Zanchetta, S., Crippa, C., Zanchi, A., &amp; Montemagni, C. (2024). The Val Biandino Intrusive Suite (central Southern Alps, N Italy): New geochronological and geochemical data on the Early Permian magmatic activity in the Southalpine Domain. <i>Swiss Journal of Geosciences,</i> <i>117</i>, 7.</p><p>Article CAS Google Scholar </p></li></ul><p>Download references<svg aria-hidden=\"true\" focusable=\"false\" height=\"16\" role=\"img\" width=\"16\"><use xlink:href=\"#icon-eds-i-download-medium\" xmlns:xlink=\"http://www.w3.org/1999/xlink\"></use></svg></p><h3>Authors and Affiliations</h3><ol><li><p>Earth Sciences Department, University of Turin, Via Valperga Caluso 35, 10125, Turin, Italy</p><p>Chiara Montomoli &amp; Salvatore Iaccarino</p></li><li><p>Institute of Earth Sciences, University of Lausanne, Géopolis Building, CH-1015, Lausanne, Switzerland</p><p>Jean-Luc Epard</p></li><li><p>Department of Geological Sciences, Stockholm University, 106 91, Stockholm, Sweden</p><p>Paola Manzotti</p></li></ol><span>Authors</span><ol><li><span>Chiara Montomoli</span>View author publications<p>You can also search for this author in <span>PubMed<span> </span>Google Scholar</span></p></li><li><span>Salvatore Iaccarino</span>View author publications<p>You can also search for this author in <span>PubMed<span> </span>Google Scholar</span></p></li><li><span>Jean-Luc Epard</span>View author publications<p>You can also search for this author in <span>PubMed<span> </span>Google Scholar</span></p></li><li><span>Paola Manzotti</span>View author publications<p>You can also search for this author in <span>PubMed<span> </span>Google Scholar</span></p></li></ol><h3>Contributions</h3><p>CM writing, editing; SI writing, editing; JLE writing, editing; PM writing, editing.</p><h3>Corresponding author</h3><p>Correspondence to Chiara Montomoli.</p><h3>Publisher's Note</h3><p>Springer Nature remains neutral with regard to jurisdictional claims in published maps and institutional affiliations.</p><p><b>Open Access</b> This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons licence, and indicate if changes were made. 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Issue: Evolution of collisional orogens in space and time—the Alpine-Himalayan system in 4 dimensions. <i>Swiss J Geosci</i> <b>117</b>, 14 (2024). https://doi.org/10.1186/s00015-024-00466-3</p><p>Download citation<svg aria-hidden=\"true\" focusable=\"false\" height=\"16\" role=\"img\" width=\"16\"><use xlink:href=\"#icon-eds-i-download-medium\" xmlns:xlink=\"http://www.w3.org/1999/xlink\"></use></svg></p><ul data-test=\"publication-history\"><li><p>Published<span>: </span><span><time datetime=\"2024-08-29\">29 August 2024</time></span></p></li><li><p>DOI</abbr><span>: </span><span>https://doi.org/10.1186/s00015-024-00466-3</span></p></li></ul><h3>Share this article</h3><p>Anyone you share the following link with will be able to read this content:</p><button data-track=\"click\" data-track-action=\"get shareable link\" data-track-external=\"\" data-track-label=\"button\" type=\"button\">Get shareable link</button><p>Sorry, a shareable link is not currently available for this 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Abstract

This Special Issue of the Swiss Journal of Geosciences entitled “Evolution of collisional orogens in space and time: the Alpine-Himalayan system in 4 dimensions”, was proposed during the joint meeting “Geosciences for a sustainable future” organized by the Società Geologica Italiana and Società Italiana di Mineralogia e Petrografia held in Turin (Italy) in September 2022.

The issue focuses on the evolution of collisional orogens through a multidisciplinary approach. As a matter of fact, continental plate collisions give rise to collisional-related orogenic belts that are some of the most spectacular and dominant features on our planet.

During collision of continental plates, considerable deformation occurs with large scale overthrusting, burial and metamorphism of continental lithosphere portions. The final anatomy and the shape of collisional belts are highly diverse, due to the interactions of several controlling factors, including the pre-collisional tectonic history, the rate and the angle of convergence, the mechanical strength and thermal state of the involved colliding plates.

The youngest collisional system on Earth is the Alpine-Himalayan belt, extending from Spain to Southeast Asia. Its general structure was first described by Emile Argand in "La tectonique de l’Asie". On the occasion of the centenary of Argand’s work, presented during the XIII International Geological congress in Belgium (August 10, 1922), this thematic volume aims to provide an updated view on the Alpine-Himalayan geology.

This Special Issue collects multidisciplinary contributions focusing on the Alpine-Himalayan system, dealing with the reconstruction of the tectonic architecture at different scales, integrating field mapping to microscale and describing the tectono-metamorphic evolution.

The papers included in this collection span from the Himalaya to the Western, Central and Ligurian Alps and also include a paper on the Alborz Mountains in Iran.

The publication by Robyr (2023) brings us in the Himalayan belt (Miyar Valley, North-West India) and focuses on the old history of the belt studying the pre-Himalayan metamorphism of the metamorphic core of the chain, until now strongly debated. Through phase petrology and microtectonics studies, combined with valuable field data, Robyr demonstrates the existence of a pre-Himalayan orogenic cycle.

Pantet et al. (2024), focus on the region surrounding the Zermatt area (SW Switzerland and NW Italy) where continental and oceanic units are strongly imbricated. Starting from a very detailed field mapping, they focus on the structure and stratigraphy of the Permian-Jurassic continent‑derived Faisceau Vermiculaire series and associated non-ophiolitic Upper Cretaceous calcschists (Série Rousse), both intercalated within ophiolitic units. They were able to reconstruct the architecture of the Briançonnais-Prepiemont palaeomargin before the onset of Alpine deformation and the structural evolution through polyphase deformation during Alpine Tectonics.

Dana et al. (2023), investigate the structural architecture and tectono-metamorphic evolution of Briançonnais units along the Ubaye–Maira valleys (South-Western Alps) at the French-Italian boundary. The Authors, starting from detailed geological mapping and integrating microstructural and metamorphic data, obtained with the Raman Spectroscopy of Carbonaceous Material, reconstruct the evolution of the subducted Briançonnais passive margin from the pre-rifting to the Alpine collisional stage.

Manna et al. (2023), present new geological data from the Ligurian Alps. The Authors, with the aid of structural mapping, UAV photogrammetric survey and digital outcrop modelling, report the first description of a 15 km-long NE-SW-striking transtensive fault network (referred to as Horse Head Fault Zone) crosscutting the metamorphic units of the area. This fault zone accommodated tens of km-scale displacements related to the Adria counterclockwise rotation after the Adria-Europe collision and the beginning of the Apennine subduction rollback.

Zanchetta et al. (2024), study the Permian Val Biandino Intrusive Suite in the central sector of the South Alpine Domain (N Italy). The Authors present new detailed petrographic, geochemical, and geochronological data of this intrusive Complex emplaced in the Variscan metamorphic basement. On the basis of their new data, they provide an updated picture of the Val Biandino Intrusive Suite, demonstrating how, despite its relatively small size, it displays a significant heterogeneity in terms of rock varieties intruded in a short time interval (ca. 5 Myrs). They conclude that the Val Biandino Intrusive Suite was likely formed through the interaction of magma generated at the mantle/crust transition and partial melting of the heterogeneous pre-Permian basement of the Southalpine Domain. These processes were linked to early Permian crustal extension and heat advection from the asthenosphere.

Rezaei et al. (2023), take us back to Asia, to the Alborz Mountains of north Iran. They investigate cumulate gabbroic rocks intruding Palaeozoic metasediments and Mesozoic sediments in the Gasht-Masuleh area. With the aid of petrographic analysis, whole-rock and mineral chemistry, as well as geochronology, the Authors were able to relate the mafic magmatism of the area to extension resulting from far-field effects linked to roll-back of the Neo-Tethys subducting slab in the mid-Cretaceous time.

Last but not least, we want to thank all the Authors who contributed to this special issue presenting their works from different sectors of the Alpine-Himalayan orogenic system. We are also very grateful to the reviewers that strongly contributed to improve the quality of the manuscripts and helped for successfully publishing this Special Issue.

Not applicable.

  • Dana, D., Iaccarino, S., Schmid, S. M., Petroccia, A., & Michard, A. (2023). Structural and metamorphic evolution of a subducted passive margin: Insights from the Briançonnais nappes of the Western Alps (Ubaye–Maira valleys, France–Italy). Swiss Journal of Geosciences, 116, 18.

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  • Manna, L., Perozzo, M., Menegoni, N., Tamburelli, S., Crispini, L., Federico, L., Seno, S., & Maino, M. (2023). Anatomy of a km-scale fault zone controlling the Oligo-Miocene bending of the Ligurian Alps (NW Italy): Integration of field and 3D high-resolution digital outcrop model data. Swiss Journal of Geosciences, 116, 15.

    Article Google Scholar

  • Pantet, A., Epard, J.-L., & Masson, H. (2024). Continent-derived metasediments (Cimes Blanches and Frilihorn) within the ophiolites around Zermatt: Relations with the Mischabel backfold and Mont Fort nappe (Pennine Alps). Swiss Journal of Geosciences, 117, 10.

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  • Rezaei, L., Timmerman, M. J., Moazzen, M., Altenberger, U., Sláma, J., Sudo, M., Günter, C., Wilke, F. D. H., & Schleicher, A. M. (2023). Mid-Cretaceous extensional magmatism in the Alborz Mountains, north Iran; geochemistry and geochronology of Gasht-Masuleh gabbros. Swiss Journal of Geosciences, 116, 14.

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  • Robyr, M. (2023). Evidence for a pre-Himalayan metamorphism in the High Himalayan Crystalline of the Miyar Valley (NW India). Swiss Journal of Geosciences, 116, 17.

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  • Zanchetta, S., Crippa, C., Zanchi, A., & Montemagni, C. (2024). The Val Biandino Intrusive Suite (central Southern Alps, N Italy): New geochronological and geochemical data on the Early Permian magmatic activity in the Southalpine Domain. Swiss Journal of Geosciences, 117, 7.

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Authors and Affiliations

  1. Earth Sciences Department, University of Turin, Via Valperga Caluso 35, 10125, Turin, Italy

    Chiara Montomoli & Salvatore Iaccarino

  2. Institute of Earth Sciences, University of Lausanne, Géopolis Building, CH-1015, Lausanne, Switzerland

    Jean-Luc Epard

  3. Department of Geological Sciences, Stockholm University, 106 91, Stockholm, Sweden

    Paola Manzotti

Authors
  1. Chiara MontomoliView author publications

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  2. Salvatore IaccarinoView author publications

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  3. Jean-Luc EpardView author publications

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  4. Paola ManzottiView author publications

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Contributions

CM writing, editing; SI writing, editing; JLE writing, editing; PM writing, editing.

Corresponding author

Correspondence to Chiara Montomoli.

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Montomoli, C., Iaccarino, S., Epard, JL. et al. Special Issue: Evolution of collisional orogens in space and time—the Alpine-Himalayan system in 4 dimensions. Swiss J Geosci 117, 14 (2024). https://doi.org/10.1186/s00015-024-00466-3

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特刊:碰撞造山运动在空间和时间上的演变--阿尔卑斯-喜马拉雅四维系统
(2023) 带我们回到亚洲,回到伊朗北部的阿尔伯兹山脉。他们研究了加什特-马苏莱赫地区侵入古生代玄武岩和中生代沉积物的辉长岩。借助岩相分析、整岩和矿物化学以及地质年代学,作者们能够将该地区的镁质岩浆活动与白垩纪中期新特提斯俯冲板块滚回所产生的远场效应导致的延伸联系起来。我们还非常感谢审稿人,他们为提高稿件质量做出了巨大贡献,并为本特刊的成功出版提供了帮助。俯冲被动边缘的结构和变质演化:来自西阿尔卑斯山脉布赖恩聪奈山系(Ubaye-Maira 山谷,法国-意大利)的启示。Swiss Journal of Geosciences, 116, 18.Article Google Scholar Manna, L., Perozzo, M., Menegoni, N., Tamburelli, S., Crispini, L., Federico, L., Seno, S., &amp; Maino, M. (2023).控制利古里亚阿尔卑斯山(意大利西北部)上新世弯曲的千米级断层带剖面图:Anomy of a km-scale fault zone controlling the Oligo-Miocene bending of the Ligurian Alps (NW Italy): integration of field and 3D high-resolution digital outcrop model data.Swiss Journal of Geosciences, 116, 15.Article Google Scholar Pantet, A., Epard, J.-L., &amp; Masson, H. (2024).采尔马特周围蛇绿混杂岩中的大陆成因变质岩(Cimes Blanches 和 Frilihorn):Relations with the Mischabel backfold and Mont Fort nappe (Pennine Alps).Swiss Journal of Geosciences, 117, 10.Article Google Scholar Rezaei, L., Timmerman, M. J., Moazzen, M., Altenberger, U., Sláma, J., Sudo, M., Günter, C., Wilke, F. D. H., &amp; Schleicher, A. M. (2023).Mid-Cretaceous extension magmatism in the Alborz Mountains, north Iran; geochemistry and geochronology of Gasht-Masuleh gabbros.Swiss Journal of Geosciences, 116, 14.Article CAS Google Scholar Robyr, M. (2023).印度西北部米亚尔山谷喜马拉雅高山结晶前变质作用的证据》。瑞士地球科学杂志》,116,17.文章 谷歌学者 Zanchetta, S., Crippa, C., Zanchi, A., &amp; Montemagni, C. (2024).Val Biandino 侵入岩组(意大利北部南阿尔卑斯山中部):关于南阿尔卑斯山岩浆活动的新地质年代和地球化学数据。瑞士地球科学杂志》,117, 7。Article CAS Google Scholar Download references作者和工作单位Earth Sciences Department, University of Turin, Via Valperga Caluso 35, 10125, Turin, ItalyChiara Montomoli &amp;Salvatore IaccarinoInstitute of Earth Sciences, University of Lausanne, Géopolis Building, CH-1015, Lausanne, SwitzerlandJean-Luc EpardDepartment of Geological Sciences, Stockholm University, 106 91, Stockholm、瑞典Paola Manzotti作者Chiara Montomoli查看作者发表的论文您也可以在PubMed Google Scholar中搜索该作者Salvatore Iaccarino查看作者发表的论文您也可以在PubMed Google Scholar中搜索该作者Jean-Luc Epard查看作者发表的论文您也可以在PubMed Google Scholar中搜索该作者Paola Manzotti查看作者发表的论文您也可以在PubMed Google Scholar中搜索该作者ContributionsCM撰写、编辑;SI撰写、编辑;JLE撰写、编辑;PM撰写、编辑。开放获取本文采用知识共享署名 4.0 国际许可协议进行许可,该协议允许以任何媒介或格式使用、共享、改编、分发和复制,只要您适当注明原作者和来源,提供知识共享许可协议的链接,并说明是否进行了修改。本文中的图片或其他第三方材料均包含在文章的知识共享许可协议中,除非在材料的署名栏中另有说明。如果材料未包含在文章的知识共享许可协议中,且您打算使用的材料不符合法律规定或超出许可使用范围,则您需要直接从版权所有者处获得许可。要查看该许可的副本,请访问 http://creativecommons.org/licenses/by/4.0/.Reprints and permissionsCite this articleMontomoli, C., Iaccarino, S., Epard, JL. et al. Special Issue:碰撞造山运动在空间和时间上的演变--阿尔卑斯-喜马拉雅四维系统。Swiss J Geosci 117, 14 (2024). https://doi.org/10.1186/s00015-024-00466-3Download citationPublished: 29 August 2024DOI: https://doi.org/10.
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来源期刊
Swiss Journal of Geosciences
Swiss Journal of Geosciences 地学-地质学
CiteScore
4.50
自引率
12.90%
发文量
21
审稿时长
>12 weeks
期刊介绍: The Swiss Journal of Geosciences publishes original research and review articles, with a particular focus on the evolution of the Tethys realm and the Alpine/Himalayan orogen. By consolidating the former Eclogae Geologicae Helvetiae and Swiss Bulletin of Mineralogy and Petrology, this international journal covers all disciplines of the solid Earth Sciences, including their practical applications. The journal gives preference to articles that are of wide interest to the international research community, while at the same time recognising the importance of documenting high-quality geoscientific data in a regional context, including the occasional publication of maps.
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