Abstract
M.Sc.
The Dabolava region is an area of approximately 600 km2 and is situated on the western edge
of the Precambrian in west-central Madagascar. The geology mainly consists of Proterozoic
amphibolite facies metavolcanic rocks, inter-layered with minor metasedimentary rocks,
crosscut by granodioritic to gabbroic plutons. The country rocks of the granodiorite and
gabbroic plutons are composed of 50% amphibolites, 30% quartzofeldspathic gneisses and
20% metasedimentary rocks, mainly carbonates. The amphibolites consist dominantly of
hornblende with plagioclase and minor quartz groundmass, although orthopyroxene,
clinopyroxene, chlorite, and biotite are present in certain samples. They have tholeiitic
affinities and may have been derived from basaltic lavas. They contain felsic segregations of
tonalitic composition that possibly represent migmatitic leucosomes, with hornblende
concentrated in associated melanosomes. The amphibolites are highly deformed compared to
the plutonic rocks. Meta-quartzofeldspathic rocks of dominant rhyolitic compositions are
interlayered within the amphibolites; these may represent felsic volcanics coeval with the
metabasalt. Metamorphosed carbonates are also interlayered within the amphibolites. This
assemblage of supracrustal rocks is intruded by Neoproterozoic granitoid and gabbroic
plutons, and granodiorite dykes. The composition of the majority of the plutons in the area of
study is mainly granodioritic, with minor quartz diorite and quartz monzodiorite. They are
metaluminous and contain quartz, plagioclase, with minor K-feldspar (microcline); biotite and
hornblende constitute the ferromagnesian minerals. The granodiorites have a prominent
foliation defined by biotite and hornblende. According to their chemical and mineralogical
composition, the granodiorites are classified as I-type in origin.
Gold mineralization is associated with the Neoproterozoic granodiorite plutons, mainly the
Dabolava and the Ambatomiefy plutons. It is hosted within quartz veins that are generally
oriented parallel to the foliation of the host rock. A limited degree of alteration is observed
within the granodiorite, with the alteration assemblages consisting of biotite, pseudomorphic
chlorite, calcite, and sericite. Gold is associated with hydrothermal biotite and sulphide
assemblages consist of pyrrhotite, arsenopyrite with minor pyrite and chalcopyrite, magnetite
and ilmenite. The chemistry of analysed gold grains from the Dabolava pluton shows that
they mainly consist of 95-97% gold with the remainder composed of Ag, Hg and Cu. A gold
concentration of up to 2232 ppm was observed in one of the gold excavations within the
Ambatomiefy pluton. Microthermometric studies reveal three fluid types, including a high
salinity fluid (type 4), a CO2-rich fluid (type 1-a), and an aqueous type (type 3). It is
suggested that the CO2-rich and high salinity fluids were exsolved from the magma. With
decreasing temperature a low salinity CO2-H2O-NaCl fluid (type 1-b, type 2) (Th ranges from
~ 220-350° C) resulted from heterogeneous mixting of a CO2-rich fluid and a low salinity
aqueous fluid. Therefore, fluid inclusion studies indicate a magmatic origin of the
mineralizing fluid(s). A porphyry-type deposit is suggested for the gold mineralization in the
study area, as it is associated with I-type granitoid plutons, the mineralizing fluid (s) are of
magmatic origin, and gold is associated with chalcopyrite, albeit in minor amounts.
Based on the rock associations observed in the field, which consist of metabasalts interlayered
with minor coeval metarhyolite, with associated intrusive plutonic rocks, as well as trace
element discrimination diagrams, an active continental margin tectonic setting is inferred for
the rocks in the study area. Two samples from the granodiorite plutons and one sample from
a gabbro body were dated using U-Pb single zircon geochronology. A sample from the
Ambatomiefy pluton yielded an age of ~1002±3 Ma, which is interpreted to represent the
crystallization age of the pluton. The Dabolava pluton has also been dated, and a similar age
of 1008 Ma has been obtained. A gabbro sample from a smaller mafic body in the area has
been dated at 982±2 Ma. This defines a ~26 m.y. period of Neoproterozoic magmatic activity.
An age of 982.3±2 .9 was also reported from a gabbro body located in the southern part of
Madagascar (Amborompotsy-Ikalamavony). These provide evidence of the presence of 1000
Ma magmatic activity in Madagascar. The extent and the significance of this magmatic event
are not yet understood although it could be related to the Mesoproterozoic event associated
with the assembly of the supercontinent Rodinia. The identification of granitoids of similar
age and character in Madagascar and within Gondwana has economic significance regarding
the potential of these granitoids for porphyry-type gold mineralization. Therefore, this is
useful for future gold exploration.