Luenha picrites, Central Mozambique – Messengers from a mantle plume source of Karoo continental flood basalts?

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Turunen , S T , Luttinen , A V , Heinonen , J S & Jamal , D L 2019 , ' Luenha picrites, Central Mozambique – Messengers from a mantle plume source of Karoo continental flood basalts? ' , Lithos , vol. 346-347 , 105152 . https://doi.org/10.1016/j.lithos.2019.105152

Title: Luenha picrites, Central Mozambique – Messengers from a mantle plume source of Karoo continental flood basalts?
Author: Turunen, Sanni T.; Luttinen, Arto V.; Heinonen, Jussi S.; Jamal, Daúd L.
Contributor: University of Helsinki, Natural Sciences Unit
University of Helsinki, University Management
University of Helsinki, Department of Geosciences and Geography
Date: 2019-11-15
Language: eng
Number of pages: 16
Belongs to series: Lithos
ISSN: 0024-4937
URI: http://hdl.handle.net/10138/306192
Abstract: We present geochemical and isotopic (Nd, Sr) data for a picrite lava suite from the Luenha River and adjacent areas in Mozambique. The Luenha picrites represent a previously unknown type of picrites related to the Karoo large igneous province (LIP) and are distinguished by their notably low TiO2 contents (0.3-1.0 wt%) and coupling of high Nb/Y with low Zr/Y and Sm/Yb. Relatively high CaO and low Zn/Fe point to a peridotitic mantle source. Contamination-sensitive incompatible element ratios show that one lava flow is likely to be uncontaminated by the crust and its composition suggests a mantle source with primitive mantle-like incompatible element ratios and mildly depleted isotopic ratios (initial Sr-87/Sr-86 = 0.7041 and epsilon(Nd) = +1.4 at 180 Ma). The primary melts of the Luenha picrites had MgO contents in the range of 13-21 wt%. Our preferred estimate for a primary melt composition (MgO = 18 wt%) resembles experimental melts of fertile mantle peridotite at 3-4 GPa and indicates liquidus temperature of 1445-1582 degrees C. Geochemical similarities suggest the Luenha picrites were generated from the same overall primitive mantle-like reservoir that produced the main volume of Karoo flood basalts in the Karoo, Kalahari, and Zambezi basins, whereas the previously identified enriched and depleted (upper) mantle sources of Karoo picrite suites (Mwenezi, Antarctica) were subordinate sources for flood basalts. We propose that the Luenha picrites record melting of a hot, chemically primitive mantle plume source that may have been rooted in the sub-African large low shear velocity province boundary and that such a source might have been the most significant magma source in the Karoo LIP. (C) 2019 The Author(s). Published by Elsevier B.V.
Subject: 1171 Geosciences
Picrite
Flood basalt
Mantle source
Large igneous province
Mantle plume
DRONNING-MAUD-LAND
LARGE IGNEOUS PROVINCE
TRACE-ELEMENT COMPOSITION
PERIDOTITE SOURCES
MELT INCLUSIONS
DEPLETED MORB
OLIVINE
ANTARCTICA
MAGMAS
LITHOSPHERE
Picrite
Flood basalt
Mantle source
Large igneous province
Mantle plume
DRONNING-MAUD-LAND
LARGE IGNEOUS PROVINCE
TRACE-ELEMENT COMPOSITION
PERIDOTITE SOURCES
MELT INCLUSIONS
DEPLETED MORB
OLIVINE
ANTARCTICA
MAGMAS
LITHOSPHERE
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