Evidences on the presence of Jurassic continental rift system in the Ravar area, Southern Tabas Block

Q: How can I download an article?

To download an article from SID, first log in to the site, search for the article title, and click on the 'Download Article' option.

Q: How can I download an ISI article?

To download an ISI article on SID, enter the keyword or article title in the search bar, view the relevant results, click on the desired article, and select the 'Download Article' option.

Q: How can I access the SID database?

To access the SID database, visit SID.ir, create an account, and log in to access scientific resources.

Q: Is downloading articles from SID free?

Some articles on SID are available for free, while others require payment. Details are specified on the article's page.

Edalati manesh Narges; Bagheri Sasan; GHOMASHI MOSTAFA; BAKHSHI MOHAMMAD REZA

مرکز اطلاعات علمی Scientific Information Database (SID) - Trusted Source for Research and Academic Resources

Journal Paper

Paper Information

Journal: TECTONICS Year:2018 | Volume:2 | Issue:5 Page(s): 37-43

Download Full-Text

Persian Verion

View:

839

Download:

Cites:

Information Journal Paper

Title

Evidences on the presence of Jurassic continental rift system in the Ravar area, Southern Tabas Block

Author(s)

Edalati manesh Narges | Bagheri Sasan | GHOMASHI MOSTAFA | BAKHSHI MOHAMMAD REZA | Issue Writer Certificate

Keywords

Rift basin

Central Iranian ophiolite

Successful rift

Kerman

Abstract

The Ravar zone, a wedge-shaped terrane, situated at the southern Tabas block, is confined between two main boundary faults, the Nayband fault in the east and the Kuhbanan fault in the west. The Mesozoic strata, especially the Jurassic layers, have a variety of facies, distribution, and exposure. Structural restoration and stratigraphical correlation between the Jurassic layers on the basis of the field and lab studies in the Ravar zone, brought new result. The stratigraphy, structure, and magmatism of the middle Jurassic to late Cretaceous successions are similar to the deposits which have been evolved in the continental rift zone is being transited to a passive margin. The sedimentary successions are classified into two groups; the clastic deposits of the Hojedk and Baghamshah Formations, and carbonate-evaporate of the Pectinid layers, and alkali basalts of the Ravar Series which are considered as the syn-rift series. The second group composed of lower Cretaceous red marl and evaporate as well as upper Cretaceous marine limestone well-thought-out as the post-rift series. These two series are separated by pronounce angular unconformity and basaltic volcanic rocks in the Ravar zone. Deepening towards the west, indicates that the main ocean, in the Cretaceous time, must be at the west side, somewhere at the west of the Tabas block. The Nain and Dehshir-Baft ophiolites could be the best candidates for the remnants of this ocean.

Cites

No record.

References

No record.

Cite

APA: Copy

Edalati manesh, Narges, Bagheri, Sasan, GHOMASHI, MOSTAFA, & BAKHSHI, MOHAMMAD REZA. (2018). Evidences on the presence of Jurassic continental rift system in the Ravar area, Southern Tabas Block. TECTONICS, 2(5 ), 37-43. SID. https://sid.ir/paper/267887/en

Vancouver: Copy

Edalati manesh Narges, Bagheri Sasan, GHOMASHI MOSTAFA, BAKHSHI MOHAMMAD REZA. Evidences on the presence of Jurassic continental rift system in the Ravar area, Southern Tabas Block. TECTONICS[Internet]. 2018;2(5 ):37-43. Available from: https://sid.ir/paper/267887/en

IEEE: Copy

Narges Edalati manesh, Sasan Bagheri, MOSTAFA GHOMASHI, and MOHAMMAD REZA BAKHSHI, “Evidences on the presence of Jurassic continental rift system in the Ravar area, Southern Tabas Block,” TECTONICS, vol. 2, no. 5 , pp. 37–43, 2018, [Online]. Available: https://sid.ir/paper/267887/en

Related Journal Papers