Dike rock generation and magma interactions in the Bir Safsaf igneous complex, south-west Egypt: Implications for the Pan-African evolution in north-east Africa

1994 ◽  
Vol 83 (3) ◽  
pp. 523-536 ◽  
Author(s):  
D. Pudlo ◽  
G. Franz
1932 ◽  
Vol 69 (5) ◽  
pp. 209-233 ◽  
Author(s):  
G. D. Osborne

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.


1922 ◽  
Vol 59 (3) ◽  
pp. 134-139 ◽  
Author(s):  
Norman L. Silvester

The area under consideration is a portion of the mountain massif bounded on the east by the Conway River, on the north by the narrow coastal plain between Conway and Bangor, and on the west and south by the popular tourist route through Nant.-Francon pass by Llyn Ogwen and down the Afon Llugwy to Bettws y coed. The investigation includes the horseshoe-shaped ring of mountains, of which the highest is Y Foel Frâs (3,091 feet), surrounding the upper course of the Aber River (Cwm yr Afon Goch). To the north-west this igneous complex is bounded by the precipitatious crags over which the above stream descends by leaps and bounds, forming the well-known Aber Falls. Upon Sheet 78, south-east of the old Geological Survey map the area is coloured as “Massive intrusive felspathic rocks”, surrounding two oval patches indicated as “Greenstones”, whilst a further elongated patch of the latter forms the south-west boundary. The north-east boundary is limited by the Aber-Llanbedr fault. Besides the hog-backed summit of Y Foel Frâs, the area includes the similarly outlined summits of Y Drosgl West (2,483 feet), Yr Arryg (2,875 feet), Llwydmor Bâch (2,256 feet), and the more rugged summits of Bera Mawr (2,587 feet), Bera Bâch and Llwydmor (2,749 feet).


1984 ◽  
Vol 22 (2) ◽  
pp. 273-285
Author(s):  
Peter Woodward

In recent years there has been a resurgence of interest in international politics in Africa. After the initial post-independence discussion of pan-Africanism the international dimension seemed overshadowed by the concern to account for domestic developments in many new states, and it is this imbalance which is now being redressed. Indeed, it has recently been argued by Robert Jackson and Carl Rosberg that, contrary to the situation elsewhere, Africa's international politics have assumed an order which is sadly lacking in the domestic affairs of many states: ‘At the level of international society, a framework of rules and conventions governing the relations of the states in the region has been bounded and sustained for almost two decades.’ If the contrast between internal anarchy and international order seems somewhat exaggerated, the distinction between domestic and foreign politics appears both conventional and appropriate.


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