Two different types of mafic dykes are found in the Muslim Bagh Ophiolite: 1) a sheeted dyke complex and 2) a mafic dyke swarm. Relative to the host plutonic section, the sheeted dykes are poorly developed, implying that they formed in an oceanic setting with a low and intermittent supply of magma, probably because of cyclic accumulation of crystals at the base of the magma chamber. Both the sheeted dykes and the dyke swarms have been metamorphosed to greenschist/amphibolite facies conditions. With the exception of the upper level gabbros and sheeted dykes, the dyke swarms crosscut almost the whole ophiolite suite as well as the metamorphic sole rocks, but are truncated structurally at the contact with the underlying mélange and sedime...
The nature, magmatic evolution, and geodynamic setting of both inner and outer Makran ophiolites, in...
Oman has two ophiolites – the better known late Cretaceous northern Oman (or Semail) ophiolite and t...
The geology of Khanozai area is comprised of Indian Platform Sediments, the Suture Zone and Flysch Z...
The geology of the Muslim Bagh area comprises the Indian passive continental margin and suture zone,...
© 2014, Saudi Society for Geosciences. Metamorphic sole rocks are exposed beneath both the Jang Tor ...
The Muslim Bagh ophiolitic complex Balochistan, Pakistan is comprised of an upper and lower nappe an...
Numerous early Cretaceous mafic and alkaline dykes, mostly trending in N-S direction, are emplaced i...
A reconnaissance survey of the 1000 Km\(^2\) of Masirah Island, Oman, has revealed a fully-developed...
The pre-Himalayan evolution of Tethys is fundamental in interpreting the signifi cance of India's Pa...
A number of Paleoproterozoic mafic dykes are reported to intrude volcano-sedimentary sequences of th...
The Bagh complex is an assemblage of igneous and sedimentary rocks containing many lithologic units...
Precambrian mafic magmatism and its role in the evolution of Earth’s crust has been paid serious att...
In this paper, we present detailed field observations, chronological, geochemical and Sr–Nd isotopic...
High-SiO2 rocks referred to as oceanic plagiogranites are common within the crustal sequences of oph...
Numerous early Cretaceous mafic and alkaline dykes, mostly trending in N-S direction, are emplaced i...
The nature, magmatic evolution, and geodynamic setting of both inner and outer Makran ophiolites, in...
Oman has two ophiolites – the better known late Cretaceous northern Oman (or Semail) ophiolite and t...
The geology of Khanozai area is comprised of Indian Platform Sediments, the Suture Zone and Flysch Z...
The geology of the Muslim Bagh area comprises the Indian passive continental margin and suture zone,...
© 2014, Saudi Society for Geosciences. Metamorphic sole rocks are exposed beneath both the Jang Tor ...
The Muslim Bagh ophiolitic complex Balochistan, Pakistan is comprised of an upper and lower nappe an...
Numerous early Cretaceous mafic and alkaline dykes, mostly trending in N-S direction, are emplaced i...
A reconnaissance survey of the 1000 Km\(^2\) of Masirah Island, Oman, has revealed a fully-developed...
The pre-Himalayan evolution of Tethys is fundamental in interpreting the signifi cance of India's Pa...
A number of Paleoproterozoic mafic dykes are reported to intrude volcano-sedimentary sequences of th...
The Bagh complex is an assemblage of igneous and sedimentary rocks containing many lithologic units...
Precambrian mafic magmatism and its role in the evolution of Earth’s crust has been paid serious att...
In this paper, we present detailed field observations, chronological, geochemical and Sr–Nd isotopic...
High-SiO2 rocks referred to as oceanic plagiogranites are common within the crustal sequences of oph...
Numerous early Cretaceous mafic and alkaline dykes, mostly trending in N-S direction, are emplaced i...
The nature, magmatic evolution, and geodynamic setting of both inner and outer Makran ophiolites, in...
Oman has two ophiolites – the better known late Cretaceous northern Oman (or Semail) ophiolite and t...
The geology of Khanozai area is comprised of Indian Platform Sediments, the Suture Zone and Flysch Z...