gtcrustГеодинамика и тектонофизикаGeodynamics & Tectonophysics2078-502XInstitute of the Earth's crust of the Russian Academy of Sciences, Siberian Branch10.5800/GT-2019-10-2-0417gtcrust-844Research ArticleПАЛЕОГЕОДИНАМИКАPALEOGEODYNAMICSМЕХАНИЗМЫ МАГМАТИЧЕСКОГО МИНГЛИНГА В КОМПОЗИТНЫХ ДАЙКАХ: МОДЕЛИ ДИСПЕРГИРОВАНИЯ И СДВИГОВОЙ ДИЛАТАЦИИMECHANISMS OF MAGMATIC MINGLING IN COMPOSITE DYKES: MODELS OF DISPERSION AND SHEAR DILATATIONhttps://orcid.org/0000-0002-2996-3789ВладимировВ. Г.VladimirovV. G.

Владимир Геннадьевич Владимиров - кандидат геолого-минералогических наук, старший научный сотрудник

630090, Новосибирск, просп. Академика Коптюга, 3, 

630090, Новосибирск, ул. Пирогова, 2

3 Academician Koptyug ave, Novosibirsk 630090, 2 Pirogov street, Novosibirsk 630090

vvg@igm.nsc.ruЯковлевВ. А.YakovlevV. A.

630090, Новосибирск, просп. Академика Коптюга, 3, 630090, Новосибирск, ул. Пирогова, 2

Vladislav A. Yakovlev - Junior Researcher

3 Academician Koptyug ave, Novosibirsk 630090, 

2 Pirogov street, Novosibirsk 630090

yakovlew.official@gmail.comКармышеваИ. В.KarmyshevaI. V.

Ирина Владимировна Кармышева - кандидат геолого-минералогических наук, научный сотрудник

630090, Новосибирск, просп. Академика Коптюга, 3, 

630090, Новосибирск, ул. Пирогова, 2

Irina V. Karmysheva - Candidate of Geology and Mineralogy, Researcher

3 Academician Koptyug ave, Novosibirsk 630090, 

2 Pirogov street, Novosibirsk 630090

iri@igm.nsc.ruИнститут геологии и минералогии им. В.С. Соболева СО РАН; Новосибирский национальный исследовательский государственный университетРоссияV.S. Sobolev Institute of Geology and Mineralogy, Siberian Branch of RAS; Novosibirsk State UniversityRussian Federation201923062019102325345Copyright © Владимиров В.Г., Яковлев В.А., Кармышева И.В., 20192019Владимиров В.Г., Яковлев В.А., Кармышева И.В.Vladimirov V.G., Yakovlev V.A., Karmysheva I.V.Данная работа распространяется под лицензией Creative Commons Attribution 4.0.This work is licensed under a Creative Commons Attribution 4.0 License.https://www.gt-crust.ru/jour/article/view/844

В работе рассматриваются вопросы интрудирования и становления комбинированных даек. Условно магматический минглинг разделен на две основные группы. Первая группа («плутоническая») – это небольшие базитовые включения, равномерно распределенные в объеме гранитоидных тел, либо вытянутые рои и шлейфы мелких тел. Вторая группа («комбинированные дайки») представлена композитными дайками, в пределах которых наблюдаются признаки механического смешения базитовых и кислых расплавов. Несмотря на сходство структурно‐текстурных особенностей и признаков механического смешения расплавов, обе группы имеют явные различия: пропорции объемов контрастных расплавов, длительность становления, место смешения расплавов, тектонические обстановки. Существующие модели не могут объяснить появление структур магматического минглинга в отдельных дайках. В данной работе вопросы механизмов смешения контрастных по составу расплавов рассмотрены на примере геологических объектов Западного Сангилена (ЦАСП). Рассмотрены общие и частные параметры комбинированных даек участков «Тавыт‐Даг» и «Сайзырал». Предложены модели сдвиговой дилатации и диспергирования для объяснения механизмов магматического минглинга в композитных дайках жильного типа.

This article is focused on the intrusion and formation of combined dykes. Two main groups of conventionally magmatic mingling are distinguished: (1) plutonic bodies, and (2) combined dykes. The first group is represented by small basite inclusions that are uniformly scattered in granitoid bodies, and includes elongated swarms and tails of small bodies. The second group includes composite dykes with the indicators of mechanical mingling of basic and acid melts. Despite the similarities in the structural and textural features and the indicators of mechanical mingling of melts, these two groups are characterized by clearly different proportions of the volumes of contrasting melts and differ in the duration of formation, place of melt mingling, and tectonic setting. None of the available models was able to explain the occurrence of magmatic mingling structures in individual dykes. In our study, the mingling mechanisms of contrasting melts are discussed using the data on the geological objects located in West Sangilen, an area of the Central Asian Orogenic Belt (CAOB). The general and specific parameters of combined dikes of the Saizyral and Tavyt‐ Dag sites are considered. The models of shear dilatation and dispersion are proposed for explaining the mechanisms of magmatic mingling in combined dykes.

минглингкомбинированная дайкасетчатая интрузиясдвиговая зонатектономагматическая эволюцияСангиленЮго‐Восточная Туваminglingcombined dikenet‐veined intrusionshear zonetectono‐magmatic evolutionSangilenSouth‐East TuvaРабота выполнена при поддержке РФФИ (проекты № 16‐05‐01011, 18‐35‐00467), ИГМ СО РАН (проект № 0330‐2016‐0003), а также Министерства образования и науки РФ (проект № 5.1688. 2017/ПЧ)ReferencesБиндеман И.Н. Ретроградная везикуляция базальтовой магмы в малоглубинных очагах: модель происхождения меланократовых включений в кислых и средних породах // Петрология. 1995. Т. 3. № 6. С. 632–644.Bindeman I.N., 1995. Retrograde vesiculation of basaltic magma in shallow foci: a model of the origin of melanocratic inclusions in acidic and middle rocks. Petrologiya (Petrology) 3 (6), 632–644 (in Russian)Burmakina G.N., Tsygankov A.A., 2013. Mafic microgranular enclaves in Late Paleozoic granitoids in the Burgasy quartz syenite massif, Western Transbaikalia: composition and petrogenesis. Petrology 21 (3), 280–303. https://doi.org/10.1134/S086959111303003X.Burmakina G.N., Tsygankov A.A., 2013. Mafic microgranular enclaves in Late Paleozoic granitoids in the Burgasy quartz syenite massif, Western Transbaikalia: composition and petrogenesis. Petrology 21 (3), 280–303. https://doi.org/10.1134/S086959111303003X.Castro A., Martino R., Vujovich G., Otamendi J., Pinotti L., D’Eramo F., Tibaldi A., Vinao A., 2008. Top-down structures of mafic enclaves within the Valle Fertil magmatic complex (Early Ordovician, San Juan, Argentina). Geologica Acta 6 (3), 217–229. https://doi.org/10.1344/105.000000252.Castro A., Martino R., Vujovich G., Otamendi J., Pinotti L., D’Eramo F., Tibaldi A., Vinao A., 2008. Top-down structures of mafic enclaves within the Valle Fertil magmatic complex (Early Ordovician, San Juan, Argentina). Geologica Acta 6 (3), 217–229. https://doi.org/10.1344/105.000000252.Cook N.D.J., 1988. Diorites and associated rocks in the Anglem Complex at The Neck, northeastern Stewart Island, New Zealand: an example of magma mingling. Lithos 21 (4), 247–262. https://doi.org/10.1016/0024-4937(88)90031-X.Cook N.D.J., 1988. Diorites and associated rocks in the Anglem Complex at The Neck, northeastern Stewart Island, New Zealand: an example of magma mingling. Lithos 21 (4), 247–262. https://doi.org/10.1016/0024-4937(88)90031-X.Didier J., Barbarin B. (Eds.), 1991. Enclaves and Granite Petrology. Developments in Petrology. Vol. 13. Elsevier, Amsterdam, 625 p.Didier J., Barbarin B. (Eds.), 1991. Enclaves and Granite Petrology. Developments in Petrology. Vol. 13. Elsevier, Amsterdam, 625 p.Dokukina K.A., Vladimirov V.G., 2005. Tectonic fragmentation of basaltic melt. Doklady Earth Sciences 401 (2), 182–186.Dokukina K.A., Vladimirov V.G., 2005. Tectonic fragmentation of basaltic melt. Doklady Earth Sciences 401 (2), 182–186.Frost T.P., Mahood G.A., 1987. Field, chemical, and physical constraints on mafic-felsic magma interaction in the Lamarck Granodiorite, Sierra Nevada, California. Geological Society of America Bulletin 99 (2), 272–291. https://doi.org/10.1130/0016-7606(1987)99<272:FCAPCO>2.0.CO;2.Frost T.P., Mahood G.A., 1987. Field, chemical, and physical constraints on mafic-felsic magma interaction in the Lamarck Granodiorite, Sierra Nevada, California. Geological Society of America Bulletin 99 (2), 272–291. https://doi.org/10.1130/0016-7606(1987)99<272:FCAPCO>2.0.CO;2.Furman T., Spera F.J., 1985. Co-mingling of acid and basic magma with implications for the origin of mafic I-type xenoliths: field and petrochemical relations of an unusual dike complex at Eagle Lake, Sequoia National Park, California, USA. Journal of Volcanology and Geothermal Research 24 (1–2), 151–178. https://doi.org/10.1016/03770273(85)90031-9.Furman T., Spera F.J., 1985. Co-mingling of acid and basic magma with implications for the origin of mafic I-type xenoliths: field and petrochemical relations of an unusual dike complex at Eagle Lake, Sequoia National Park, California, USA. Journal of Volcanology and Geothermal Research 24 (1–2), 151–178. https://doi.org/10.1016/03770273(85)90031-9.Gamble J.A., 1979. Some relationships between coexisting granitic and basaltic magmas and the genesis of hybrid rocks in the Tertiary central complex of Slieve Gullion, northeast Ireland. Journal of Volcanology and Geothermal Research 5 (3–4), 297–316. https://doi.org/10.1016/0377-0273(79)90021-0.Gamble J.A., 1979. Some relationships between coexisting granitic and basaltic magmas and the genesis of hybrid rocks in the Tertiary central complex of Slieve Gullion, northeast Ireland. Journal of Volcanology and Geothermal Research 5 (3–4), 297–316. https://doi.org/10.1016/0377-0273(79)90021-0.Huppert H.E., Sparks S.J., 1988. The generation of granitic magmas by intrusion of basalt into continental crust. Journal of Petrology 29 (3), 599–624. https://doi.org/10.1093/petrology/29.3.599.Huppert H.E., Sparks S.J., 1988. The generation of granitic magmas by intrusion of basalt into continental crust. Journal of Petrology 29 (3), 599–624. https://doi.org/10.1093/petrology/29.3.599.Изох А.Э., Лавренчук А.В., Васюкова Е.А. Дайковый комплекс Западного Сангилена – проявление ордовикского мантийного магматизма // Геодинамическая эволюция литосферы Центрально-Азиатского подвижного пояса (от океана к континенту). Вып. 2. Иркутск: Изд-во Института географии СО РАН, 2004. Т. 1. С. 143–144.Izokh A.E., Lavrenchuk A.V., Vasyukova E.A., 2004. The dike complex of West Sangilen is a manifestation of the Ordovician mantle magmatism. In: Geodynamic evolution of the lithosphere of the Central Asian mobile belt (from ocean to continent). Issue 2, Vol. 1. Publishing House of the Institute of Geography SB RAS, Irkutsk, p. 143–144 (in Russian)Karmysheva I.V., Vladimirov V.G., Vladimirov A.G., Shelepaev R.A., Yakovlev V.A., Vasyukova E.A., 2015. Tectonic position of mingling dykes in accretion-collision system of Early Caledonides of West Sangilen (South-East Tuva, Russia). Geodinamics & Tectonophysics 6 (3), 289–310. https://doi.org/10.5800/GT-2015-6-3-0183.Karmysheva I.V., Vladimirov V.G., Vladimirov A.G., Shelepaev R.A., Yakovlev V.A., Vasyukova E.A., 2015. Tectonic position of mingling dykes in accretion-collision system of Early Caledonides of West Sangilen (South-East Tuva, Russia). Geodinamics & Tectonophysics 6 (3), 289–310. https://doi.org/10.5800/GT-2015-6-3-0183.Хромых С.В., Бурмакина Г.Н., Цыганков А.А., Котлер П.Д., Владимиров А.Г. Взаимодействие габброидной и гранитоидной магм при формировании Преображенского интрузива, Восточный Казахстан // Геодинамика и тектонофизика. 2017. Т. 8. № 2. С. 311–330. https://doi.org/10.5800/GT-2017-8-2-0243.Khromykh S.V., Burmakina G.N., Tsygankov А.А., Kotler P.D., Vladimirov A.G., 2017. Interactions between gabbroid and granitoid magmas during formation of the Preobrazhensky intrusion, East Kazakhstan. Geodynamics & Tectonophysics 8 (2), 311–330 (in Russian) https://doi.org/10.5800/GT-2017-8-2-0243.Кузьмичев А.Б. Тектоническая история Тувино-Монгольского массива: раннебайкальский, позднебайкальский и раннекаледонский этапы. М.: Пробел-2000, 2004. 191 с..Kuzmichev A.B., 2004. Tectonic History of the Tuva-Моngоliа Massif: Early Baikalian, Late Baikalian and Early Caledonian Stages. PROBEL-2000, Moscow, 191 р. (in Russian)Kuzmichev A.B., Bibikova E.V., Zhuravlev D.Z., 2001. Neoproterozoic (similar to 800 Ma) orogeny in the Tuva-Mongolia Massif (Siberia): island arc-continent collision at the northeast Rodinia margin. Precambrian Research 110 (1–4), 109–126. https://doi.org/10.1016/S0301-9268(01)00183-8.Kuzmichev A.B., Bibikova E.V., Zhuravlev D.Z., 2001. Neoproterozoic (similar to 800 Ma) orogeny in the Tuva-Mongolia Massif (Siberia): island arc-continent collision at the northeast Rodinia margin. Precambrian Research 110 (1–4), 109–126. https://doi.org/10.1016/S0301-9268(01)00183-8.Литвиновский Б.А., Занвилевич А.Н., Калманович М.А. Многократное смешение сосуществующих сиенитовых и базитовых магм и его петрологическое значение, Усть Хилокский массив, Забайкалье // Петрология. 1995. Т. 3. № 2. С. 133–157.Litvinovsky B.A., Zanvilevich A.N., Kalmanovich M.A., 1995a. Repeated mixing of coexisting syenitic and basic magmas and its petrological significance, Ust-Khilok massif, Transbaikalia. Petrologiya 3 (2), 133–157 (in Russian)Литвиновский Б.А., Занвилевич А.Н., Ляпунов С.М., Биндеман И.Н., Дэвис А.М., Калманович М.А. Условия образования комбинированных базит-гранитных даек (Шалутинский массив, Забайкалье) // Геология и геофизика. 1995. Т. 36. № 7. С. 3–22.Litvinovsky B.A., Zanvilevich A.N., Lyapunov S.M., Bindeman I.N., Davis A.M., Kalmanovich M.A., 1995b. Model of composite basite-granitoid dike generation (Shaluta Pluton, Transbaikalia). Geologiya i Geofizika (Russian Geology and Geophysics) 36 (7), 3–22 (in Russian)Litvinovsky B.A., Zanvilevich A.N., Wickham S.M., Jahn B.M., Vapnik Y., Kanakin S.V., Karmanov N.S., 2017. Composite dikes in four successive granitoid suites from Transbaikalia, Russia: The effect of silicic and mafic magma interaction on the chemical features of granitoids. Journal of Asian Earth Sciences 136, 16–39. https://doi.org/10.1016/j.jseaes.2016.12.037.Litvinovsky B.A., Zanvilevich A.N., Wickham S.M., Jahn B.M., Vapnik Y., Kanakin S.V., Karmanov N.S., 2017. Composite dikes in four successive granitoid suites from Transbaikalia, Russia: The effect of silicic and mafic magma interaction on the chemical features of granitoids. Journal of Asian Earth Sciences 136, 16–39. https://doi.org/10.1016/j.jseaes.2016.12.037.Lowell G.R., Young G.J., 1999. Interaction between coeval mafic and felsic melts in the St. Francois Terrane of Missouri, USA. Precambrian Research 95 (1–2), 69–88. https://doi.org/10.1016/S0301-9268(98)00127-2.Lowell G.R., Young G.J., 1999. Interaction between coeval mafic and felsic melts in the St. Francois Terrane of Missouri, USA. Precambrian Research 95 (1–2), 69–88. https://doi.org/10.1016/S0301-9268(98)00127-2.Marshall L.A., Sparks R.S.J., 1984. Origin of some mixed-magma and net-veined ring intrusions. Journal of the Geological Society 141 (1), 171–182. https://doi.org/10.1144/gsjgs.141.1.0171.Marshall L.A., Sparks R.S.J., 1984. Origin of some mixed-magma and net-veined ring intrusions. Journal of the Geological Society 141 (1), 171–182. https://doi.org/10.1144/gsjgs.141.1.0171.Nardi L.V.S., de Lima E.F., 2000. Hybridisation of mafic microgranular enclaves in the Lavras Granite Complex, southern Brazil. Journal of South American Earth Sciences 13 (1–2), 67–78. https://doi.org/10.1016/S0895-9811(00)00006-7.Nardi L.V.S., de Lima E.F., 2000. Hybridisation of mafic microgranular enclaves in the Lavras Granite Complex, southern Brazil. Journal of South American Earth Sciences 13 (1–2), 67–78. https://doi.org/10.1016/S0895-9811(00)00006-7.Perugini D., Poli G., 2005. Viscous fingering during replenishment of felsic magma chambers by continuous inputs of mafic magmas: Field evidence and fluid-mechanics experiments. Geology 33 (1), 5–8. https://doi.org/10.1130/G21075.1.Perugini D., Poli G., 2005. Viscous fingering during replenishment of felsic magma chambers by continuous inputs of mafic magmas: Field evidence and fluid-mechanics experiments. Geology 33 (1), 5–8. https://doi.org/10.1130/G21075.1.Полянский О.П., Семенов А.Н., Владимиров В.Г., Кармышева И.В., Владимиров А.Г., Яковлев В.А. Численная модель магматического минглинга (на примере Баянкольской габбро‐гранитной серии, Сангилен, Тува) // Геодинамика и тектонофизика. 2017. Т. 8. № 2. С. 385–403. https://doi.org/10.5800/GT-2017-8-2-0247.Polyansky O.P., Semenov A.N., Vladimirov V.G., Karmysheva I.V., Vladimirov A.G., Yakovlev V.A., 2017. Numerical simulation of magma mingling (case of Bayankol gabbro‐granite series, Sangilen, Tuva). Geodynamics & Tectonophysics 8 (2), 385–403 (in Russian) https://doi.org/10.5800/GT-2017-8-2-0247.Sklyarov E.V., Fedorovskii V.S., 2006. Magma mingling: tectonic and geodynamic implications. Geotectonics 40 (2), 120–134. https://doi.org/10.1134/S001685210602004X.Sklyarov E.V., Fedorovskii V.S., 2006. Magma mingling: tectonic and geodynamic implications. Geotectonics 40 (2), 120–134. https://doi.org/10.1134/S001685210602004X.Tsygankov A.A., Burmakina G.N., Yakovlev V.A., Khubanov V.B., Vladimirov V.G., Karmysheva I.V., Buyantuev M.D., 2019. Composition and U-Pb (LA-ICP-MS) isotopic age of zircons from composite dikes of Western Sangilen (TuvaMongolian orogen). Russian Geology and Geophysics 60 (1), 45–66. https://doi.org/10.15372/RGG2019004.Tsygankov A.A., Burmakina G.N., Yakovlev V.A., Khubanov V.B., Vladimirov V.G., Karmysheva I.V., Buyantuev M.D., 2019. Composition and U-Pb (LA-ICP-MS) isotopic age of zircons from composite dikes of Western Sangilen (TuvaMongolian orogen). Russian Geology and Geophysics 60 (1), 45–66. https://doi.org/10.15372/RGG2019004.Владимиров В.Г. Происхождение и механизмы формирования структур магматического минглинга в комбинированных габбро-гранитных дайках // Петрология магматических и метаморфических комплексов: Материалы IX Всероссийской петрографической конференции с международным участием. Томск: ТГУ, 2017. С. 67–69.Vladimirov V.G., 2017. The origin and mechanisms of formation of magmatic mingling structures in combined gabbro-granite dykes. In: Petrology of magmatic and metamorphic complexes. Materials of the IX All-Russia petrographic conference with international participation. Tomsk State University, Tomsk, p. 67–69 (in Russian)Владимиров В.Г., Кармышева И.В., Яковлев В.А. Две группы магматического минглинга (на примере ранних каледонид Западного Сангилена, ЮгоВосточная Тува) // Корреляция алтаид и уралид: магматизм, метаморфизм, стратиграфия, геохронология, геодинамика 22>_ë2Ä_F!и металлогения: Материалы Третьей международной научной конференции. Новосибирск: Изд-во СО РАН, 2016. С. 52–53.Vladimirov V.G., Karmysheva I.V., Yakovlev V.A., 2016. Two groups of magmatic mingling (case of the early caledonides of West Sangilen, Southeastern Tuva). In: Correlation of Altaides and Uralides: magmatism, metamorphism, stratigraphy, geochronology, geodynamics and metallogeny. Materials of the Third International scientific conference. Publishing House of SB RAS, Novosibirsk, p. 52–53 (in Russian)Владимиров В.Г., Кармышева И.В., Яковлев В.А., Травин А.В., Цыганков А.А., Бурмакина Г.Н. Термохронология минглинг‐даек Западного Сангилена (Юго‐Восточная Тува): свидетельства развала коллизионной системы на северо‐западной окраине Тувино‐Монгольского массива // Геодинамика и тектонофизика. 2017. Т. 8. № 2. С. 283–310. https://doi.org/10.5800/GT-2017-8-2-0242.Vladimirov V.G., Karmysheva I.V., Yakovlev V.А., Travin А.V., Tsygankov А.А., Burmakina G.N., 2017. Thermochronology of mingling dykes in West Sangilen (South‐East Tuva, Russia): evidence of the collapse of the collisional system in the north‐western edge of the Tuva‐Mongolia massif. Geodynamics & Tectonophysics 8 (2), 283–310 (in Russian) https://doi.org/10.5800/GT-2017-8-2-0242.Vladimirov V.G., Vladimirov A.G., Gibsher A.S., Travin A.V., Rudnev S.N., Shemelina I.V., Barabash N.V., Savinykh Y.V., 2005. Model of the tectonometamorphic evolution for the Sangilen block (southeastern Tuva, Central Asia) as a reflection of the Early Caledonian accretion-collision tectogenesis. Doklady Earth Sciences 405 (8), 1159–1165.Vladimirov V.G., Vladimirov A.G., Gibsher A.S., Travin A.V., Rudnev S.N., Shemelina I.V., Barabash N.V., Savinykh Y.V., 2005. Model of the tectonometamorphic evolution for the Sangilen block (southeastern Tuva, Central Asia) as a reflection of the Early Caledonian accretion-collision tectogenesis. Doklady Earth Sciences 405 (8), 1159–1165.Wiebe R.A., 1973. Relations between coexisting basaltic and granitic magmas in a composite dike. American Journal of Science 273 (2), 130–151. https://doi.org/10.2475/ajs.273.2.130.Wiebe R.A., 1973. Relations between coexisting basaltic and granitic magmas in a composite dike. American Journal of Science 273 (2), 130–151. https://doi.org/10.2475/ajs.273.2.130.Wilcox R.E., 1999. The idea of magma mixing: history of a struggle for acceptance. The Journal of Geology 107 (4), 421–432. https://doi.org/10.1086/314357.Wilcox R.E., 1999. The idea of magma mixing: history of a struggle for acceptance. The Journal of Geology 107 (4), 421–432. https://doi.org/10.1086/314357.Windley B.F., 1965. The composite net-veined diorite intrusives of the Julianehå b district, South Greenland. Meddelelser om Grønland 172 (8), 1–60.Windley B.F., 1965. The composite net-veined diorite intrusives of the Julianehå b district, South Greenland. Meddelelser om Grønland 172 (8), 1–60.Занвилевич А.Н., Калманович М.А., Литвиновский Б.А., Посохов В.Ф., Шадаев М.Г. Раннепермский этап гранитоидного магматизма в Западном Забайкалье // Геология и геофизика. 1991. Т. 32. № 11. С. 27–37.Zanvilevich A.N., Kalmanovich M.A., Litvinovsky B.A., Posokhov V.F., Shadaev M.G., 1991. Early Permian stage of granitoid magmatic activity in the Western Transbaikalia. Geologiya i Geofizika (Russian Geology and Geophysics) 32 (11), 27–37 (in Russian)Zimanowski B., Büttner R., 2002. Dynamic mingling of magma and liquefied sediments. Journal of Volcanology and Geothermal Research 114 (1–2), 37–44. https://doi.org/10.1016/S0377-0273(01)00281-5.Zimanowski B., Büttner R., 2002. Dynamic mingling of magma and liquefied sediments. Journal of Volcanology and Geothermal Research 114 (1–2), 37–44. https://doi.org/10.1016/S0377-0273(01)00281-5.

The authors declare that there are no conflicts of interest present.