Tourmalinization in the Astaneh granitoids (south west Arak)

Transcription

Tourmalinization in the Astaneh granitoids (south west Arak)
Vol. 17, No. 3 Fall 1388/2009
Tourmalinization in the Astaneh granitoids (south west Arak)
*
Z. Tahmasbi1 , A. Ahmadi Khalaji 2, M. Rajaeieh3
1- Department of Mining, Faculty of Engineering, University of Lorestan, Lorestan, Iran
2- Department of Geology, Faculty of Sciences, University of Lorestan, Khorramabad, Iran
3- Department of Geology, Faculty of Sciences, University of Isfahan, Isfahan, Iran
(Received: 25/12/2008, in revised form: 6/4/2009)
Abstract: The studied area is a small portion of Sanandaj – Sirjan zone. Metasomatism at the
contact of intrusive body studied and penetration of Al-rich rocks caused tourmalinization to
stratiform tourmalinite in pelitic hornfels. In addition, hydrothermal fluids crystallized tourmaline
nodules in monzogranite surface. The Fe/ (Fe + Mg) ratio in varied between 0.4-0.76 in
stratiform tourmaline and 0.83-0.96 in tourmaline nodules respectively. The tourmaline
composition is schorlite- dravite. Chemical zoning in this mineral show that system is open and
crystallization is unequilibrium. The flat trace end rare earth elements imply to mobility of LREE
induced to alteration that this phenomena occur to increasing HREE/ LREE in this type
tourmalines.
Keywords: Astaneh, microprobe, metasomatism, Sanandaj- Sirjan zone, tourmaline.
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Corresponding author, Tel.: +98 (0661) 3349083, Fax:+98 (0661) 6200005, E-mail: [email protected]
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