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A new plumbing system framework for mantle plume-related continental Large Igneous Provinces and their mafic-ultramafic intrusions

Ernst, R.E., Liikane, D.A., Jowitt, S.M., Buchan, K.L., Blanchard, J.A.·2019·Journal of Volcanology and Geothermal Research
DOI 10.1016/j.jvolgeores.2019.07.007
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Fig. 1 Framework for the plumbing system of continental large igneous provinces (LIPs) associated with mantle plumes: A) cross section, B) paleosurface plan view. C) subsurface plan view. Magmaticunits are colored by type of unit: magmatic underplate (purple), mafic-ultramafic intrusion (blue), mafic sills (black), radiating mafic dykes (brown), circumferential mafic dykes (red), and flood basalts (green). Associated units include silicic magmatism (pink). carbonatites (purple triangles), and kimberlites (purple circles). Red star indicates mantle plume center location and scales are typical, although LIP events can be both smaller and larger than depicted. Letters provide a link to key discussion points in the text. Note, thicker lithosphere on the right side of the cross section which would prevent mafic magmatism on that side of the plume and thus prevent circumferential dykes on that side (see gap in circumferential pattern on upper right side of part B).
Fig. 1 Framework for the plumbing system of continental large igneous provinces (LIPs) associated with mantle plumes: A) cross section, B) paleosurface plan view. C) subsurface plan view. Magmaticunits are colored by type of unit: magmatic underplate (purple), mafic-ultramafic intrusion (blue), mafic sills (black), radiating mafic dykes (brown), circumferential mafic dykes (red), and flood basalts (green). Associated units include silicic magmatism (pink). carbonatites (purple triangles), and kimberlites (purple circles). Red star indicates mantle plume center location and scales are typical, although LIP events can be both smaller and larger than depicted. Letters provide a link to key discussion points in the text. Note, thicker lithosphere on the right side of the cross section which would prevent mafic magmatism on that side of the plume and thus prevent circumferential dykes on that side (see gap in circumferential pattern on upper right side of part B).CC-BY-NC-ND · From the PDF

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Cited by

See all 139

Metadata

Authors
Ernst, R. E., Liikane, D. A., Jowitt, S. M., Buchan, K. L., & Blanchard, J. A.
Venue
Journal of Volcanology and Geothermal Research
Publisher
Elsevier BV
Published
2019-10
Volume
384
Pages
75-84
ISSN
0377-0273
DOI
10.1016/j.jvolgeores.2019.07.007
Cited by
139
References
1
Language
en
Licence
Funders
  • МЕГАГРАНТЫ
  • Natural Sciences and Engineering Research Council of Canada (523131-17)

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