Add to ORKG第8回極域科学シンポジウム/個別セッション：[OG] 極域地圏12月6日（水）国立極地研究所 3階セミナー室The Eighth Symposium on Polar Science/Ordinary sessions: [OG] Polar GeosciencesWed. 6 Dec./3F Seminar room, National Institute of Polar Researc
The Neoproterozoic rocks of the Bir Madi area, south eastern desert, comprise a Metagabbro-Diorite C...
The Neoproterozoic rock assemblages in the Wadi Hafafit Culmination (WHC) can be subdivided into two...
The Kid Group is one of the few exposures of Neoproterozoic metavolcano-sedimentary rocks in the bas...
Banded iron formation (BIF) is exposed among the Precambrian rocks in the Wadi Karim and Um Anab are...
In the central Eastern Desert of Egypt, deposits of iron-formation of the Algoma type occur as sharp...
The petrography of the Precambrian iron-bearing formation at Wadi Kareim proved that the formation c...
This paper deals with the geological and geochemical characterization of ironstone deposits encounte...
The Abu Dabbab albite granite (ADAG), in the central Eastern Desert of Egypt, hosts the most signifi...
a b s t r a c t Submarine tholeiitic and calc-alkaline basalt and andesite with subordinate dacite, ...
Neoproterozoic iron formation (NIF) provides evidence for the widespread return of anoxic and ferrug...
The Late Neoproterozoic basement exposures in the Sinai Peninsula and Eastern Desert of Egypt repres...
Major and trace element compositions of samples of Banded Iron Formations (BIF) from the Neoarchaean...
Abstract – Dyke swarms traverse Neoproterozoic rocks in the Hawashiya region in the extreme northern...
In Egypt, mafic-ultramafic complexes have been classified into three major types: incomplete ophioli...
The Eastern Desert (ED) Neoproterozoic ophiolites are tectonically important elements of the Arabian...
The Neoproterozoic rocks of the Bir Madi area, south eastern desert, comprise a Metagabbro-Diorite C...
The Neoproterozoic rock assemblages in the Wadi Hafafit Culmination (WHC) can be subdivided into two...
The Kid Group is one of the few exposures of Neoproterozoic metavolcano-sedimentary rocks in the bas...
Banded iron formation (BIF) is exposed among the Precambrian rocks in the Wadi Karim and Um Anab are...
In the central Eastern Desert of Egypt, deposits of iron-formation of the Algoma type occur as sharp...
The petrography of the Precambrian iron-bearing formation at Wadi Kareim proved that the formation c...
This paper deals with the geological and geochemical characterization of ironstone deposits encounte...
The Abu Dabbab albite granite (ADAG), in the central Eastern Desert of Egypt, hosts the most signifi...
a b s t r a c t Submarine tholeiitic and calc-alkaline basalt and andesite with subordinate dacite, ...
Neoproterozoic iron formation (NIF) provides evidence for the widespread return of anoxic and ferrug...
The Late Neoproterozoic basement exposures in the Sinai Peninsula and Eastern Desert of Egypt repres...
Major and trace element compositions of samples of Banded Iron Formations (BIF) from the Neoarchaean...
Abstract – Dyke swarms traverse Neoproterozoic rocks in the Hawashiya region in the extreme northern...
In Egypt, mafic-ultramafic complexes have been classified into three major types: incomplete ophioli...
The Eastern Desert (ED) Neoproterozoic ophiolites are tectonically important elements of the Arabian...
The Neoproterozoic rocks of the Bir Madi area, south eastern desert, comprise a Metagabbro-Diorite C...
The Neoproterozoic rock assemblages in the Wadi Hafafit Culmination (WHC) can be subdivided into two...
The Kid Group is one of the few exposures of Neoproterozoic metavolcano-sedimentary rocks in the bas...