The Kukuluma Intrusive Complex (KIC) is a late Archean igneous complex, dominated by monzonite and diorite with subordinated granodiorite. The monzonite and the diorite suites have low silica content (SiO2≤62 wt%), moderate Mg# (Mg#average=49), high Sr/Y (Sr/Yaverage=79) and high La/Yb (La/Ybaverage=56) ratios, and strongly fractionated (Lan/Ybn=9–69) REE patterns. Their moderate Ni (Niaverage=50 ppm), Cr (Craverage=85 ppm), variable Cr/Ni ratio (0.65–3.56) and low TiO2 (TiO2average=0.5 wt%) indicate little to no interaction with the peridotitic mantle. For most major elements (Al2O3, FeOt, Na2O, TiO2 and P2O5) the monzonite and the diorite suites display subparallel trends for the same SiO2 content indicating they represent distinct melts....
The Geita Greenstone Belt is a late Archean greenstone belt located in the Tanzania Craton, trending...
Tertiary and later igneous activity is common on and around the Tanzanian craton, with primitive mag...
Insight into the formation of Archean trondhjemite–tonalite–granodiorite (TTG) and sanukitoids is es...
The Kukuluma Intrusive Complex (KIC) is a late Archean igneous complex, dominated by monzonite and d...
Granitoids intruding the late Archaean sequences of the Sukumaland Greenstone Belt of northern Tanza...
Petrography, mineral major- and trace element analyses and Rb–Sr and Sm–Nd systematics of xenoliths ...
The Kapalagulu and Musongati intrusions are differentiated mafic–ultramafic intrusions, more than 1 ...
peer reviewedA succession of mafic-ultramafic layered intrusions forms an alignment in the boundary ...
The Kapalagulu and Musongati intrusions are differentiated mafic–ultramafic intrusions, more than 1 ...
Granitoids intruding the late Archaean sequences of the Sukumaland Greenstone Belt of northern Tanza...
The Merelani-Lelatema area, which is occupied by late Proterozoic metasedimentary rocks, lies along ...
Sillimanite/kyanite + K-feldspar + quartz ± garnet + biotite ± Fe-Ti oxide-bearing rocks occur assoc...
Mg-rich metabasalts from the Simba Sirori to Majimoto segment of the southern Musoma-Mara greenstone...
New isotopic (Sm–Nd) and geochemical data are presented for volcano-sedimentary and granitic lithoty...
There is a pronounced occurrence of gabbroic rocks in the western part of the Lupa gold field, SW Ta...
The Geita Greenstone Belt is a late Archean greenstone belt located in the Tanzania Craton, trending...
Tertiary and later igneous activity is common on and around the Tanzanian craton, with primitive mag...
Insight into the formation of Archean trondhjemite–tonalite–granodiorite (TTG) and sanukitoids is es...
The Kukuluma Intrusive Complex (KIC) is a late Archean igneous complex, dominated by monzonite and d...
Granitoids intruding the late Archaean sequences of the Sukumaland Greenstone Belt of northern Tanza...
Petrography, mineral major- and trace element analyses and Rb–Sr and Sm–Nd systematics of xenoliths ...
The Kapalagulu and Musongati intrusions are differentiated mafic–ultramafic intrusions, more than 1 ...
peer reviewedA succession of mafic-ultramafic layered intrusions forms an alignment in the boundary ...
The Kapalagulu and Musongati intrusions are differentiated mafic–ultramafic intrusions, more than 1 ...
Granitoids intruding the late Archaean sequences of the Sukumaland Greenstone Belt of northern Tanza...
The Merelani-Lelatema area, which is occupied by late Proterozoic metasedimentary rocks, lies along ...
Sillimanite/kyanite + K-feldspar + quartz ± garnet + biotite ± Fe-Ti oxide-bearing rocks occur assoc...
Mg-rich metabasalts from the Simba Sirori to Majimoto segment of the southern Musoma-Mara greenstone...
New isotopic (Sm–Nd) and geochemical data are presented for volcano-sedimentary and granitic lithoty...
There is a pronounced occurrence of gabbroic rocks in the western part of the Lupa gold field, SW Ta...
The Geita Greenstone Belt is a late Archean greenstone belt located in the Tanzania Craton, trending...
Tertiary and later igneous activity is common on and around the Tanzanian craton, with primitive mag...
Insight into the formation of Archean trondhjemite–tonalite–granodiorite (TTG) and sanukitoids is es...