PETROLOGY, GEOCHEMISTRY AND GEODYNAMIC SETTING OF GABBROIC SUBVOLCANICS IN THE WEST OF SHAFARUD, TALESH MOUNTAINS

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.

KESHAVARZ HEDAYATI M.; EMAMI M.H.; KARIMI BAVAND POUR A.R.; BAHAR FIROUZI KH.

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

Journal Paper

Paper Information

Journal: GEOSCIENCES Year:2015 | Volume:24 | Issue:95 (PETROLOGY & MINERALOGY) Page(s): 155-164

Download Full-Text

Persian Verion

View:

999

Download:

Cites:

Information Journal Paper

Title

PETROLOGY, GEOCHEMISTRY AND GEODYNAMIC SETTING OF GABBROIC SUBVOLCANICS IN THE WEST OF SHAFARUD, TALESH MOUNTAINS

Author(s)

KESHAVARZ HEDAYATI M. | EMAMI M.H. | KARIMI BAVAND POUR A.R. | BAHAR FIROUZI KH. | Issue Writer Certificate

Keywords

MICROGABBROIC SILLS AND DIKESQ2

SHAFARUDQ2

ASTHENOSPHEREQ2

Abstract

The MICROGABBROIC SILLS AND DIKES have injected into the late Cretaceous limestones along SHAFARUD. Based on the textural and mineralogical features, they are divided into four groups: micro olivine gabbro, microgabbro, microgabbro-diorite, and diabase. The main minerals in these rocks are olivine, clinopyroxene, amphibole, and plagioclase. The spider diagrams show that the primary mafic magma is probably originated from the ASTHENOSPHERE, but due to contamination with upper continental crust during eruption has been modified to calc-alkaline. As a result, depletion of Nb and enrichment in Pb, Rb, Cs, Th, and U is observed. Discrimination diagrams show that the primary alkaline microgabbros influenced by AFC process and modified to calc-alkaline rocks. The presences of pyroclastic enclaves in diabasic rocks indicate that the diabasic rocks are younger than the pyroclastic rocks.

Cites

No record.

References

No record.

Cite

APA: Copy

KESHAVARZ HEDAYATI, M., EMAMI, M.H., KARIMI BAVAND POUR, A.R., & BAHAR FIROUZI, KH.. (2015). PETROLOGY, GEOCHEMISTRY AND GEODYNAMIC SETTING OF GABBROIC SUBVOLCANICS IN THE WEST OF SHAFARUD, TALESH MOUNTAINS. GEOSCIENCES, 24(95 (PETROLOGY & MINERALOGY)), 155-164. SID. https://sid.ir/paper/31736/en

Vancouver: Copy

KESHAVARZ HEDAYATI M., EMAMI M.H., KARIMI BAVAND POUR A.R., BAHAR FIROUZI KH.. PETROLOGY, GEOCHEMISTRY AND GEODYNAMIC SETTING OF GABBROIC SUBVOLCANICS IN THE WEST OF SHAFARUD, TALESH MOUNTAINS. GEOSCIENCES[Internet]. 2015;24(95 (PETROLOGY & MINERALOGY)):155-164. Available from: https://sid.ir/paper/31736/en

IEEE: Copy

M. KESHAVARZ HEDAYATI, M.H. EMAMI, A.R. KARIMI BAVAND POUR, and KH. BAHAR FIROUZI, “PETROLOGY, GEOCHEMISTRY AND GEODYNAMIC SETTING OF GABBROIC SUBVOLCANICS IN THE WEST OF SHAFARUD, TALESH MOUNTAINS,” GEOSCIENCES, vol. 24, no. 95 (PETROLOGY & MINERALOGY), pp. 155–164, 2015, [Online]. Available: https://sid.ir/paper/31736/en

Related Journal Papers