Geochronology, geochemistry, and Hf–Sr-Nd isotopes of the Hamisana Shear Zone granitoids in northeastern Sudan: Petrogenesis and tectonic evolution of neoproterozoic juvenile crust in the Nubian Shield

2020 ◽  
Vol 347 ◽  
pp. 105857
Author(s):  
Adil Saeed ◽  
Zuoxun Zeng ◽  
Yildirim Dilek ◽  
S.F. Awadelseid ◽  
A.A. Abdel Rahman ◽  
...  
2015 ◽  
Vol 51 (4) ◽  
pp. 670-681 ◽  
Author(s):  
Vincenzo Festa ◽  
Giacomo Prosser ◽  
Alfredo Caggianelli ◽  
Antonietta Grande ◽  
Antonio Langone ◽  
...  

2021 ◽  
Author(s):  
A Zagorevski ◽  
C R van Staal ◽  
J H Bédard ◽  
A Bogatu ◽  
D Canil ◽  
...  

Ophiolite complexes are an important component of oceanic terranes in the northern Cordillera and constitute a significant amount of juvenile crust added to the Mesozoic Laurentian continental margin during Cordilleran orogenesis. Despite their tectonic importance, few systematic studies of these complexes have been conducted. Detailed studies of the pseudostratigraphy, age, geochemistry, and structural setting of ophiolitic rocks in the northern Cordillera indicate that ophiolites formed in Permian to Middle Triassic suprasubduction zone settings and were obducted onto passive margin sequences. Re-evaluation of ophiolite complexes highlights fundamental gaps in the understanding of the tectonic framework of the northern Cordillera. The previous inclusion of ophiolite complexes into generic 'oceanic' terranes resulted in significant challenges for stratigraphic nomenclature, led to incorrect terrane definitions, and resulted in flawed tectonic reconstructions.


2020 ◽  
Vol 13 (21) ◽  
Author(s):  
Abdelhamid El Fakharani ◽  
Abdelhady Radwan ◽  
Mohammed Hassan Younis ◽  
Ashraf Emam ◽  
Sherif Fawzy

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