ANALOGOUS TECTONIC EVOLUTION OF THE TETHYAN AND SE ASIAN REGIONS

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.

SHAHABPOUR J.

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

Journal Paper

Paper Information

Journal: IRANIAN JOURNAL OF SCIENCE AND TECHNOLOGY TRANSACTION A- SCIENCE Year:2009 | Volume:33 | Issue:A1 Page(s): 57-64

Download Full-Text

Persian Verion

View:

599

Download:

708

Cites:

Information Journal Paper

Title

ANALOGOUS TECTONIC EVOLUTION OF THE TETHYAN AND SE ASIAN REGIONS

Author(s)

SHAHABPOUR J. | Issue Writer Certificate

Keywords

TETHYAN REGIONQ3

SE ASIAN REGIONQ3

ANALOGOUS TECTONIC EVOLUTIONQ3

Abstract

The study of tectonic evolution of the Tethyan and SE ASIAN REGIONs indicates that these two regions have each passed through southwardly progressing sequences of similar tectonic events. Both regions have experienced a southward island-arc subduction and back-arc spreading leading to continental detachment from Gondwanaland, with an earlier southward island arc subduction of Palaeotethys (Tethyan northern ocean), and continental detachment (Early Devonian) which produced the Neo-Tethys Ocean and the land masses of the TETHYAN REGION, compared with a later southward island arc subduction of Tethys II, and continental detachment (Permo-Triassic) which produced Tethys III, and the land masses of the SE ASIAN REGION. The northward subduction of Neo-Tethys (Tethyan southern ocean) and formation of the Alpine Orogeny (Late Paleocene-Pliocene) in the TETHYAN REGION was accompanied by the opening of the Red Sea to the south of the Arabian Gondwanaland. Similarly, the northward subduction of Tethys III (SE Asian southern ocean) (Late Oligocene-Present), and arc-continent collision in the SE ASIAN REGION was accompanied by the opening of the Southern Ocean to the south of the Australian Gondwanaland. In both regions, the younger oceans are formed sequentially southward. The later occurrence of the southward progressing sequence of tectonic events in the SE ASIAN REGION compared with the similar sequence of tectonic events in the TETHYAN REGION indicates an eastward global migration of tectonic events.

Cites

No record.

References

No record.

Cite

APA: Copy

SHAHABPOUR, J.. (2009). ANALOGOUS TECTONIC EVOLUTION OF THE TETHYAN AND SE ASIAN REGIONS. IRANIAN JOURNAL OF SCIENCE AND TECHNOLOGY TRANSACTION A- SCIENCE, 33(A1), 57-64. SID. https://sid.ir/paper/117888/en

Vancouver: Copy

SHAHABPOUR J.. ANALOGOUS TECTONIC EVOLUTION OF THE TETHYAN AND SE ASIAN REGIONS. IRANIAN JOURNAL OF SCIENCE AND TECHNOLOGY TRANSACTION A- SCIENCE[Internet]. 2009;33(A1):57-64. Available from: https://sid.ir/paper/117888/en

IEEE: Copy

J. SHAHABPOUR, “ANALOGOUS TECTONIC EVOLUTION OF THE TETHYAN AND SE ASIAN REGIONS,” IRANIAN JOURNAL OF SCIENCE AND TECHNOLOGY TRANSACTION A- SCIENCE, vol. 33, no. A1, pp. 57–64, 2009, [Online]. Available: https://sid.ir/paper/117888/en

Related Journal Papers