PETROLOGY AND GEODYNAMICS OF YOUNG DOMES AND OTHER ASSOCIATED SUB - VOLCANIC BODIES OF BALADEH (CENTRAL ALBORZ - IRAN)

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.

EMAMI MOHAMMAD HASHEM; NOURI ZADEH MOHAMMAD

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

Journal Paper

Paper Information

Journal: GEOSCIENCES Year:2007 | Volume:16 | Issue:62 Page(s): 80-101

Download Full-Text

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

Persian Verion

View:

953

Download:

Cites:

Information Journal Paper

Title

PETROLOGY AND GEODYNAMICS OF YOUNG DOMES AND OTHER ASSOCIATED SUB - VOLCANIC BODIES OF BALADEH (CENTRAL ALBORZ - IRAN)

Author(s)

EMAMI MOHAMMAD HASHEM | NOURI ZADEH MOHAMMAD | Issue Writer Certificate

Keywords

VOLCANIC DOMESQ3

PETROLOGYQ2

GEODYNAMICSQ3

IGNEOUS DIAPIRISMQ3

RHYOLITEQ2

DACITEQ2

DIKEQ2

SILLQ2

CENTRAL ALBORZQ2

BALADEHQ2

Abstract

Young VOLCANIC DOMES and other associated sub-volcanic bodies of BALADEH (Central Alborz) have reached the surface passing through Shemshak Formation (Jurassic). Most of acidic domes and bodies (dacite, RHYOLITE, and rhyo-dacite) have extruded relatively cold and possess some surficial features. Petrological, textural, and geochemical similarities all over the surface of these domes indicate that they have an endogenous history. According to modern geodynamic models, all of these volcanic rocks are derived from one feeding DIKE (along Haraz River) which has been dissected after passing the brittle-ductile boundary. Some of the pieces of DIKEs can be traced in the 2nd and 3rd locations (east of Ba ladeh village and south of Valashid village). Convergent (collision or post-orogenic) condition is the best scenario for tectonic setting of these bodies based on geochemical data. In addition to partial melting, some other processes such as crustal contamination, gas transfer and to some extent alteration were effective genetic processes. LILE and LREE enrichment patterns indicate low degree of partial melting or end products of fractional crystallization and some crustal contamination (Ba enrichment).

Cites

No record.

References

No record.

Cite

APA: Copy

EMAMI, MOHAMMAD HASHEM, & NOURI ZADEH, MOHAMMAD. (2007). PETROLOGY AND GEODYNAMICS OF YOUNG DOMES AND OTHER ASSOCIATED SUB - VOLCANIC BODIES OF BALADEH (CENTRAL ALBORZ - IRAN). GEOSCIENCES, 16(62), 80-101. SID. https://sid.ir/paper/31914/en

Vancouver: Copy

EMAMI MOHAMMAD HASHEM, NOURI ZADEH MOHAMMAD. PETROLOGY AND GEODYNAMICS OF YOUNG DOMES AND OTHER ASSOCIATED SUB - VOLCANIC BODIES OF BALADEH (CENTRAL ALBORZ - IRAN). GEOSCIENCES[Internet]. 2007;16(62):80-101. Available from: https://sid.ir/paper/31914/en

IEEE: Copy

MOHAMMAD HASHEM EMAMI, and MOHAMMAD NOURI ZADEH, “PETROLOGY AND GEODYNAMICS OF YOUNG DOMES AND OTHER ASSOCIATED SUB - VOLCANIC BODIES OF BALADEH (CENTRAL ALBORZ - IRAN),” GEOSCIENCES, vol. 16, no. 62, pp. 80–101, 2007, [Online]. Available: https://sid.ir/paper/31914/en

Related Journal Papers