Ti-Rich Tholeiitic Picrites from the Prinsen af Wales Bjerge, East Greenland, and Evidence for a Pyroxene-Rich Mantle Source at Breakup in the North Atlantic
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Ti-Rich Tholeiitic Picrites from the Prinsen af Wales Bjerge, East Greenland, and Evidence for a Pyroxene-Rich Mantle Source at Breakup in the North Atlantic. / Hansen, Henriette; Nielsen, Troels F. D.
I: Journal of Petrology, Bind 63, Nr. 8, egac078, 2022.Publikation: Bidrag til tidsskrift › Tidsskriftartikel › Forskning › fagfællebedømt
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T1 - Ti-Rich Tholeiitic Picrites from the Prinsen af Wales Bjerge, East Greenland, and Evidence for a Pyroxene-Rich Mantle Source at Breakup in the North Atlantic
AU - Hansen, Henriette
AU - Nielsen, Troels F. D.
PY - 2022
Y1 - 2022
N2 - Highly magnesian, olivine-phyric tholeiitic basaltic and picritic lavas with >5 wt% TiO2 from the Prinsen af Wales Bjerge (PAWB) region are chemically distinct from all other Paleogene East Greenland flood basalts and from basalts in the North Atlantic Igneous Province. The similar to 100-m-thick lava succession rests on the 61 Ma Urbjerget Formation, is intercalated with volcaniclastic sediments, and has 57 Ma 40Ar/39Ar stepwise degassing ages. It is part of the Milne Land Formation, the first of the major flood basalt formations in East Greenland, and the result of plume impingement of the Kangerlussuaq area in East Greenland during the initial stages of continental breakup. The Ti-rich picrites have relatively primitive compositions and contain Mn- and Ni-rich olivine up to Fo(88). Intermediate to high Sr-87/Sr-86(i) (0.7034-0.7044) and low Pb isotopic compositions reflect 4-11% crustal contamination, whereas the initial epsilon Nd (+4 - +5) and Os-187/Os-188 ratios (0.121-0.129) overlap with recent Icelandic basalts and appear little affected by contamination processes. The mantle source of the Ti-rich picrites contained garnet and was pyroxene-rich and similar to that of later low-Si alkaline basalts. The Ti-rich picrites of the PAWB, similar to other Ti-rich melts of the Kangerlussuaq region, represent analogies of MgO-rich and variably TiO2-enriched melts from pyroxene rich sources of traditionally accepted mantle plumes like Hawaii.
AB - Highly magnesian, olivine-phyric tholeiitic basaltic and picritic lavas with >5 wt% TiO2 from the Prinsen af Wales Bjerge (PAWB) region are chemically distinct from all other Paleogene East Greenland flood basalts and from basalts in the North Atlantic Igneous Province. The similar to 100-m-thick lava succession rests on the 61 Ma Urbjerget Formation, is intercalated with volcaniclastic sediments, and has 57 Ma 40Ar/39Ar stepwise degassing ages. It is part of the Milne Land Formation, the first of the major flood basalt formations in East Greenland, and the result of plume impingement of the Kangerlussuaq area in East Greenland during the initial stages of continental breakup. The Ti-rich picrites have relatively primitive compositions and contain Mn- and Ni-rich olivine up to Fo(88). Intermediate to high Sr-87/Sr-86(i) (0.7034-0.7044) and low Pb isotopic compositions reflect 4-11% crustal contamination, whereas the initial epsilon Nd (+4 - +5) and Os-187/Os-188 ratios (0.121-0.129) overlap with recent Icelandic basalts and appear little affected by contamination processes. The mantle source of the Ti-rich picrites contained garnet and was pyroxene-rich and similar to that of later low-Si alkaline basalts. The Ti-rich picrites of the PAWB, similar to other Ti-rich melts of the Kangerlussuaq region, represent analogies of MgO-rich and variably TiO2-enriched melts from pyroxene rich sources of traditionally accepted mantle plumes like Hawaii.
KW - Ti-rich picrites
KW - East Greenland
KW - flood basalt
KW - pyroxene-rich mantle source
KW - HETEROGENEOUS ICELAND PLUME
KW - ISOTOPIC EVIDENCE
KW - GARDINER COMPLEX
KW - GEOCHEMICAL CONSTRAINTS
KW - PHASE-EQUILIBRIA
KW - PERIDOTITE KLB-1
KW - OXYGEN FUGACITY
KW - FLOOD BASALTS
KW - HIGH-MG
KW - TERTIARY
U2 - 10.1093/petrology/egac078
DO - 10.1093/petrology/egac078
M3 - Journal article
VL - 63
JO - Journal of Petrology
JF - Journal of Petrology
SN - 0022-3530
IS - 8
M1 - egac078
ER -
ID: 344974958