[HTML][HTML] Orogen styles in the East African Orogen: A review of the Neoproterozoic to Cambrian tectonic evolution

H Fritz, M Abdelsalam, KA Ali, B Bingen… - Journal of African Earth …, 2013 - Elsevier
Abstract The East African Orogen, extending from southern Israel, Sinai and Jordan in the
north to Mozambique and Madagascar in the south, is the world́s largest Neoproterozoic to …

The supercontinent cycle: a retrospective essay

RD Nance, JB Murphy, M Santosh - Gondwana Research, 2014 - Elsevier
The recognition that Earth history has been punctuated by supercontinents, the assembly
and breakup of which have profoundly influenced the evolution of the geosphere …

[图书][B] Geology of Western Gondwana (2000-500 Ma): Pan-African-Brasiliano Aggregation of South America and Africa (translated by AV Carozzi, Univ. of Illinois, USA …

R Trompette - 2020 - taylorfrancis.com
In considering the geology of Western Gondwana, this text covers: the Pan-African-
Brasiliano cratons; the Pan-African-Brasiliano fold belts; and amosaic of Pan-African …

A synopsis of events related to the assembly of eastern Gondwana

JG Meert - Tectonophysics, 2003 - Elsevier
The assembly of the eastern part of Gondwana (eastern Africa, Arabian–Nubian shield
(ANS), Seychelles, India, Madagascar, Sri Lanka, East Antarctica and Australia) resulted …

Plume-generated triple junctions: key indicators in applying plate tectonics to old rocks

K Burke, JF Dewey - The Journal of Geology, 1973 - journals.uchicago.edu
Continental lithosphere-especially where stationary with respect to mantle plumes-is marked
by plume-generated uplifts typically crested by volcanoes that rupture in three rifts at angles …

[图书][B] Earth as an evolving planetary system

KC Condie - 2021 - books.google.com
Earth as an Evolving Planetary System, Fourth Edition discusses key topics dealing with the
evolution and interaction through time of Earth's crust, mantle, core, atmosphere …

Crustal evolution in the East African Orogen: a neodymium isotopic perspective

RJ Stern - Journal of African Earth Sciences, 2002 - Elsevier
The East African Orogen (EAO) is one of Earth's great collision zones, where East and West
Gondwana collided to form the supercontinentGreater Gondwana'orPannotia'at the end of …

Continuation of the Mozambique Belt into East Antarctica: Grenville-age metamorphism and polyphase Pan-African high-grade events in central Dronning Maud Land

J Jacobs, CM Fanning, F Henjes-Kunst… - The Journal of …, 1998 - journals.uchicago.edu
The about 500 km long coastal stretch of central Dronning Maud Land (DML), East
Antarctica, is critical for understanding both Gondwana and Rodinia assembly. In common …

Ophiolites in Northeast and East Africa: implications for Proterozoic crustal growth

SM Berhe - Journal of the Geological Society, 1990 - lyellcollection.org
The presence of ophiolite complexes in NE and E Africa has been documented using
Landsat, field and geochemical studies. The present work identifies five major ophiolitic …

Geological development of the rift system of eastern Africa

RB McConnell - Geological Society of America Bulletin, 1972 - pubs.geoscienceworld.org
Abstract The active East African Rift System forms a belt of anastomosing faults extending
4,000 km south-southwest from the junction of the Red Sea and Gulf of Aden to the Zambezi …