Initial Reports of the Deep Sea Drilling Project 1974
DOI: 10.2973/dsdp.proc.23.123.1974
|View full text |Cite
|
Sign up to set email alerts
|

Sedimentary History of the Red Sea

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
2
1
1

Citation Types

2
20
0

Year Published

1978
1978
2018
2018

Publication Types

Select...
4
4

Relationship

0
8

Authors

Journals

citations
Cited by 28 publications
(24 citation statements)
references
References 19 publications
2
20
0
Order By: Relevance
“…However, the carbonate-free fractions of sediments from active ridges are depleted in Al and Si, indicating that the absolute quantities of clay minerals are small . Such a mixture of smectites has been reported for Red Sea sediments (Stoffers and Ross, 1974). In two of the East Pacific Rise sediments investigated here, both di-and tri octahedral clays probably are present.…”
supporting
confidence: 79%
“…However, the carbonate-free fractions of sediments from active ridges are depleted in Al and Si, indicating that the absolute quantities of clay minerals are small . Such a mixture of smectites has been reported for Red Sea sediments (Stoffers and Ross, 1974). In two of the East Pacific Rise sediments investigated here, both di-and tri octahedral clays probably are present.…”
supporting
confidence: 79%
“…The Marmara Sea is forming as a pull-apart basin along the North Anatolian Fault (Armijo et al, 1999(Armijo et al, , 2002. Direct connection with the Indian Ocean is definitively closed and the question of the connection with the Red Sea might be discussed but the presence of Messinian evaporites in the Red Sea (Stoffers and Ross, 1974) suggests that the absolute sea level was very low and thus makes the possibility of a passage to the Mediterranean unlikely (Rouchy, 1986). Temporary connections with the Eastern Paratethys are proposed through the northern Aegean .…”
Section: Langhian -Serravallian (Fig 2d and E)mentioning
confidence: 97%
“…In the late Miocene the connection between the Mediterranean and Red seas was interrupted (Stoffers and Ross, 1974). The Suez Isthmus was a highland from the late Miocene to Pliocene (Said, 1962).…”
Section: Geological History Of the Suez Isthmusmentioning
confidence: 98%