Geochemistry and Nd isotopic composition of potassic magmatism in the Neoarchaean Musoma-Mara greenstone belt, northern Tanzania
Manya Shukrani; Maboko Makenya, A.H.; Nakamura Eizo
Precambrian Research 159(3-4): 231-240
2007
ISSN/ISBN: 0301-9268
DOI: 10.1016/j.precamres.2007.07.001
Accession: 022712596
The Neoarchaean Musoma-Mara Greenstone Belt (MMGB) of northern Tanzania is underlain in part by the approximately 2649 Ma post-orogenic potassic-rich granites, which are the most abundant intrusive rocks in the belt. The rocks are composed of plagioclase+K-feldspar+quartz+biotite + or - sphene + or - zircon + or - hornblende + or - chlorite. They are characterized by high contents of SiO (sub 2) (68.90-77.76 wt%), K (sub 2) O (3.71-5.44 wt%) and low Na (sub 2) O (3.27-5.70 wt%) leading to low ratios of Na (sub 2) O/K (sub 2) O (0.63-1.02). The rocks are depleted in CaO (0.22-2.41 wt%) as well as in Sr (15-412 ppm), Cr (< or =16 ppm) and Ni (< or =5 ppm); and their major element composition are similar to those of experimental melts derived from partial melting of tonalite. On chondrite-normalized REE patterns, these rocks show fractionated patterns (La/Yb (sub CN) = 1.22-41.32) that are characterised by moderate to strongly negative Eu anomalies (Eu/Eu (super *) = 0.04-0.86). On primitive mantle-normalized spidergrams, these rocks are generally enriched in Th, U, K and Pb and depleted in Ba, Sr, Nb, Ta and Ti relative to adjacent elements. The K-rich granites have epsilon Nd (sub o) (at 2.649 Ga) values of +0.55 to +1.70 that compare well with those of associated volcanic rocks and TTG (epsilon Nd = +0.44 to +2.66) which predate the emplacement of the K-rich granitoids. Their mean crustal residence ages are 170 to 450 Ma older than their emplacement ages. The overall geochemical features of this suite of rocks, together with evidence from experimental results, are consistent with their generation by partial melting of relatively juvenile igneous rocks within the continental crust at pressures corresponding to depths <15 km where plagioclase was a stable phase. The transition from earlier TTG magmatism to potassic magmatism in the MMGB is interpreted as marking a transition from growth of the Neoarchaean continental crust through the addition of juvenile mantle-derived material to intra-crustal recycling of pre-existing material.