The Lower Cretaceous Giant Dyke Swarms in the Arctic and Its Significance for linking of Siberia-Iceland Hot-Spot Track

<正>Siberia-Iceland hot-spot track is the one of hot-spot track preserved on continent.Although this hot-spot track has clear plume"heads"-Siberia large igneous province,owing to thick continental lithosphere,its continuing S1 36

Bibliographic Details
Main Authors: LIU Zhonglan, LI Jianghai, ZHANG Huatian
Other Authors: The Key Laboratory of Orogenic Belts and Crustal Evolution, School of Earth and Space Sciences, Peking University
Format: Journal/Newspaper
Language:English
Published: Acta Geologica Sinica(English Edition) 2016
Subjects:
Siberia
continent
Cretaceous
Giant
preserved
thick
Arctic
continuing
linking
Lower
Iceland
Online Access:https://hdl.handle.net/20.500.11897/479954
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spelling ftpekinguniv:oai:localhost:20.500.11897/479954 2023-05-15T14:40:44+02:00 The Lower Cretaceous Giant Dyke Swarms in the Arctic and Its Significance for linking of Siberia-Iceland Hot-Spot Track LIU Zhonglan LI Jianghai ZHANG Huatian The Key Laboratory of Orogenic Belts and Crustal Evolution School of Earth and Space Sciences Peking University 2016 https://hdl.handle.net/20.500.11897/479954 en eng Acta Geologica Sinica(English Edition) Acta Geologica Sinica(English Edition). 2016, 36. 1926592 1000-9515 http://hdl.handle.net/20.500.11897/479954 知网 Siberia continent Cretaceous Giant preserved thick Arctic continuing linking Lower Journal 2016 ftpekinguniv https://doi.org/20.500.11897/479954 2021-08-01T11:17:49Z <正>Siberia-Iceland hot-spot track is the one of hot-spot track preserved on continent.Although this hot-spot track has clear plume"heads"-Siberia large igneous province,owing to thick continental lithosphere,its continuing S1 36 Journal/Newspaper Arctic Iceland Siberia Peking University Institutional Repository (PKU IR) Arctic
institution Open Polar
collection Peking University Institutional Repository (PKU IR)
op_collection_id ftpekinguniv
language English
topic Siberia
continent
Cretaceous
Giant
preserved
thick
Arctic
continuing
linking
Lower
spellingShingle Siberia
continent
Cretaceous
Giant
preserved
thick
Arctic
continuing
linking
Lower
LIU Zhonglan
LI Jianghai
ZHANG Huatian
The Lower Cretaceous Giant Dyke Swarms in the Arctic and Its Significance for linking of Siberia-Iceland Hot-Spot Track
topic_facet Siberia
continent
Cretaceous
Giant
preserved
thick
Arctic
continuing
linking
Lower
description <正>Siberia-Iceland hot-spot track is the one of hot-spot track preserved on continent.Although this hot-spot track has clear plume"heads"-Siberia large igneous province,owing to thick continental lithosphere,its continuing S1 36
author2 The Key Laboratory of Orogenic Belts and Crustal Evolution
School of Earth and Space Sciences
Peking University
format Journal/Newspaper
author LIU Zhonglan
LI Jianghai
ZHANG Huatian
author_facet LIU Zhonglan
LI Jianghai
ZHANG Huatian
author_sort LIU Zhonglan
title The Lower Cretaceous Giant Dyke Swarms in the Arctic and Its Significance for linking of Siberia-Iceland Hot-Spot Track
title_short The Lower Cretaceous Giant Dyke Swarms in the Arctic and Its Significance for linking of Siberia-Iceland Hot-Spot Track
title_full The Lower Cretaceous Giant Dyke Swarms in the Arctic and Its Significance for linking of Siberia-Iceland Hot-Spot Track
title_fullStr The Lower Cretaceous Giant Dyke Swarms in the Arctic and Its Significance for linking of Siberia-Iceland Hot-Spot Track
title_full_unstemmed The Lower Cretaceous Giant Dyke Swarms in the Arctic and Its Significance for linking of Siberia-Iceland Hot-Spot Track
title_sort lower cretaceous giant dyke swarms in the arctic and its significance for linking of siberia-iceland hot-spot track
publisher Acta Geologica Sinica(English Edition)
publishDate 2016
url https://hdl.handle.net/20.500.11897/479954
geographic Arctic
geographic_facet Arctic
genre Arctic
Iceland
Siberia
genre_facet Arctic
Iceland
Siberia
op_source 知网
op_relation Acta Geologica Sinica(English Edition). 2016, 36.
1926592
1000-9515
http://hdl.handle.net/20.500.11897/479954
op_doi https://doi.org/20.500.11897/479954
_version_ 1766312578267480064

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