Geological sketch map of the north-western Melfi plutonic massif.

Geological sketch map of the north-western Melfi plutonic massif.

Source publication
Article
Full-text available
This paper presents petrographic and geochemical data on magmatic rocks of the north-western Melfi massif (part of the Gera Massif at the center of Chad) in the Adamawa-Yadé domain. The study area consists of syenite and granite, all crosscut by minor dykes and quartz veins. Syenite and granite show porphyritic texture and are dominated by K-feldsp...

Contexts in source publication

Context 1
... samples of the different rocks studied here have been collected at the north-western Melfi region in Chad (Fig. 2). For the petrographic study, thin sections were done at the thin section laboratory, Department of earth science, University of Yaoundé I (Cameroon). These thin sections have been described at the Cartography Geochemistry and Metallogeny Laboratory, Department of Earth Sciences, University of Ngaoundéré (Cameroon). Whole-rock ...
Context 2
... (B01, B04, MG4, GERF, CG1) were identified in the vicinity of Gogmi, Boudia, Mogol, and Gerfen (Fig. 2). They crop out as subcircular plutons, characterized by medium altitudes ranging between 480 and 680 m. In Gogmi area, rock is crosscut by quartz veins with metric length and variable thickness (1 to 10 cm). In all the localities mentioned above, the rock is pink to grey, has massive structure, and is fine-to-coarse grained. At the ...

Similar publications

Article
Full-text available
The Mangling intrusive complex has different dioritic to granitic phases and is spatially and temporally related to molybdenum deposits in the Qinling Orogen. Zircon U-Pb dating of the Mangling intrusive complex indicates that dioritic rocks (biotite diorite and biotite diorite enclave; ca. 150−147 Ma) formed earlier than granitic rocks (medium- to...
Article
Full-text available
The early Paleozoic magmatic rocks are widespread in the West Kunlun orogenic belt, and their formation is genetically linked to subduction-collision of the Proto-Tethys ocean. However, the petrogenesis of these magmatic rocks and their tectonic setting remain controversial. In this paper, we present new zircon U–Pb ages, whole-rock geochemistry, S...
Article
Full-text available
Ospinsk is an area in Russia well-known for mining the highest quality green nephrite in the world. However, the chatoyant green nephrite found here has not been studied to date. This study explores the mineralogy, geochemistry, and petrogenesis of chatoyant green nephrite collected from Ospinsk using polarizing microscope back-scattered electron i...
Chapter
Full-text available
The Varėna suite is spatial and plausibly genetic association of ultramafic rocks, composed of olivine, orthopyroxene, clinopyroxene, magnetite, dolomite and apatite, substituted in different degrees by serpentine, amphiboles, phlogopite. These rocks form complex bodies, which occupy few square kilometres on the surface of the crystalline basement....