GEOCHEMISTRY AND U-PB DATING OF NORTH SAMANGRANITOID ROCKS

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HOSSEINI B.; AHMADI A.R.

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Journal: GEOSCIENCES Year:2016 | Volume:25 | Issue:100 Page(s): 109-120

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Information Journal Paper

Title

GEOCHEMISTRY AND U-PB DATING OF NORTH SAMANGRANITOID ROCKS

Author(s)

HOSSEINI B. | AHMADI A.R. | Issue Writer Certificate

Keywords

SANANDAJ-SIRJAN ZONEQ2

SAMANQ2

GRANITOIDQ1

U-PB DATINGQ2

GEOCHEMISTRYQ1

JURASSICQ2

Abstract

Deformed GRANITOID rocks from North SAMAN represent part of magmatic activity in the SANANDAJ-SIRJAN ZONE during the Mesozoic. The GRANITOID rocks intruded as separate intrusions into the metamorphic rocks with protolith ages of the Palaeozoic and Mezosoic. These GRANITOIDs are deformed as a result of subsequent tectonic activities. Zircon U-Pb ages of crystals separated from the GRANITOID rocks gave ages of 182 ± 4 Ma and indicate that the GRANITOID rocks crystallized at the Toarcian stage of the lower JURASSIC. The major and trace element goechemistry suggests a subduction-related, active continental margin setting for the GRANITOID bodies. The occurrences of numerous JURASSIC GRANITOIDs reveal the importance of magmatic activities during this period in the SANANDAJ-SIRJAN ZONE.

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APA: Copy

HOSSEINI, B., & AHMADI, A.R.. (2016). GEOCHEMISTRY AND U-PB DATING OF NORTH SAMANGRANITOID ROCKS. GEOSCIENCES, 25(100), 109-120. SID. https://sid.ir/paper/31701/en

Vancouver: Copy

HOSSEINI B., AHMADI A.R.. GEOCHEMISTRY AND U-PB DATING OF NORTH SAMANGRANITOID ROCKS. GEOSCIENCES[Internet]. 2016;25(100):109-120. Available from: https://sid.ir/paper/31701/en

IEEE: Copy

B. HOSSEINI, and A.R. AHMADI, “GEOCHEMISTRY AND U-PB DATING OF NORTH SAMANGRANITOID ROCKS,” GEOSCIENCES, vol. 25, no. 100, pp. 109–120, 2016, [Online]. Available: https://sid.ir/paper/31701/en

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