1972
DOI: 10.1038/235144a0
|View full text |Cite
|
Sign up to set email alerts
|

Tectonic Significance of the Afar (or Danakil) Depression

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
2
1
1
1

Citation Types

0
24
1

Year Published

1982
1982
2022
2022

Publication Types

Select...
6
4

Relationship

0
10

Authors

Journals

citations
Cited by 95 publications
(25 citation statements)
references
References 18 publications
0
24
1
Order By: Relevance
“…This is similar in size, morphology, and spacing to second order, non-transform offset segmentation of slow spreading mid-oceanic ridges (Hayward and Ebinger, 1996). The southward advance of the SSW-trend along Erta Ale-Manda Hararo is broken into shorter rift and magmatic segments that are arranged into rift-in-rift structure as they approach the Tendaho and Gobaad axial ranges further south (Tazieff and Varet, 1972).…”
Section: The Manda Hararo-gobaad Riftmentioning
confidence: 93%
“…This is similar in size, morphology, and spacing to second order, non-transform offset segmentation of slow spreading mid-oceanic ridges (Hayward and Ebinger, 1996). The southward advance of the SSW-trend along Erta Ale-Manda Hararo is broken into shorter rift and magmatic segments that are arranged into rift-in-rift structure as they approach the Tendaho and Gobaad axial ranges further south (Tazieff and Varet, 1972).…”
Section: The Manda Hararo-gobaad Riftmentioning
confidence: 93%
“…3c; Tazieff et al, 1971;Barberi and Varet, 1977;Varet, 1978). Rifting at Asal (Delibrias et al, 1975) connected these structures to the Gulf of Tadjoura, separating the Danakil block from the rest of Afar (Figs.…”
Section: Quaternary Geology and Neotectonicsmentioning
confidence: 96%
“…1A), covering a distance of about 110 km. It passes south of the Danakil Alps, which are composed of Mesozoic basement and are thought to have separated from the Ethiopian plateau by a 10-18 rotation around a pole in the Gulf of Zula during the past 4 Myr (Tazieff et al 1972;Sichler 1980;Souriot and Brun 1992). Several volcanoes make up the range, including Sork'Ale, the caldera complexes of Bara'Ale, Mallahle, and Nabro itself, which at 2,248 m marks the highest point in the NVR, the silicic domes of Mabda, Dubbi, the Edd lava field, and Kod Ali island located in the Red Sea (Fig.…”
Section: The Nabro Volcanic Range (Nvr)mentioning
confidence: 99%