Permian felsic magmatism in the Neoproterozoic Nagar Parkar Igneous Complex of the Malani Igneous Suite: Evidence from zircon U–Pb age

Island Arc ◽  
2019 ◽  
Vol 28 (6) ◽  
Author(s):  
Hafiz U. Rehman ◽  
Tahseenullah Khan ◽  
Hao‐Yang Lee ◽  
Sun‐Lin Chung ◽  
Mamoru Murata ◽  
...  
Keyword(s):  
Igneous Complex ◽  
Malani Igneous Suite

MULTIPLE SULFUR ISOTOPES IN GRANITE-HOSTED SULFIDES FROM THE BUSHVELD IGNEOUS COMPLEX

2017 ◽  
Author(s):  
Travis Lewis Steiner-Leach ◽  
◽  
Maureen Feineman ◽  
Sarah Penniston-Dorland ◽  
Nivea Magalhaes ◽  
...  
Keyword(s):  
Sulfur Isotopes ◽  
Igneous Complex ◽  
Bushveld Igneous Complex ◽  
Multiple Sulfur Isotopes

Surficial geochemical and mineralogical signatures of Ni-Cu-PGE deposits in glaciated terrain: examples from the South Range of the Sudbury Igneous Complex, Ontario, Canada

2021 ◽  
pp. 104301
Author(s):  
Sarah Hashmi ◽  
Matthew I. Leybourne ◽  
Daniel Layton-Matthews ◽  
Stewart Hamilton ◽  
M. Beth McClenaghan ◽  
...  
Keyword(s):  
The South ◽  
Igneous Complex ◽  
Sudbury Igneous Complex

The Metamorphosed Limestones and Associated Contaminated Igneous Rocks of the Carlingford District, Co. Louth

1932 ◽  
Vol 69 (5) ◽  
pp. 209-233 ◽  
Author(s):  
G. D. Osborne
Keyword(s):  
Igneous Rocks ◽  
The South ◽  
Ordnance Survey ◽  
Igneous Complex ◽  
North East ◽  
The North ◽  
South West ◽  
Carboniferous Limestone ◽  
Contamination Effects

THE Carlingford-Barnave district falls within the boundaries of Sheet 71 of the Ordnance Survey of Ireland, and forms part of a broad promontory lying between Carlingford Lough on the north-east and Dundalk Bay on the south-west. The greater part of this promontory is made up of an igneous complex of Tertiary age which has invaded the Silurian slates and quartzites and the Carboniferous Limestone Series. This complex has not yet been investigated in detail, but for the purposes of the present paper certain references to it are necessary, and these are made below. The prevalence of hybrid-relations and contamination-effects between the basic and acid igneous rocks of the region is a very marked feature, and because of this it has been difficult at times to decide which types have been responsible for the various stages of the metamorphism.

scholarly journals Arc–continent collision and the formation of continental crust: a new geochemical and isotopic record from the Ordovician Tyrone Igneous Complex, Ireland

2009 ◽  
Vol 166 (3) ◽  
pp. 485-500 ◽  
Author(s):  
Amy E. Draut ◽  
Peter D. Clift ◽  
Jeffrey M. Amato ◽  
Jerzy Blusztajn ◽  
Hans Schouten
Keyword(s):  
Continental Crust ◽  
Igneous Complex
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