PETROGRAPHY AND GEOCHEMISTRY OF MINERALS IN FELDSPATHOID- BEARING ROCKS, LOCATED IN NORTH SHAHR-BABAK, WEST MEIDUK VILLAGE

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.

MORADIAN A.

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

Journal Paper

Paper Information

Journal: Iranian Journal of Crystallography and Mineralogy Year:2006 | Volume:13 | Issue:2 Page(s): 215-228

Download Full-Text

Persian Verion

View:

702

Download:

Cites:

Information Journal Paper

Title

PETROGRAPHY AND GEOCHEMISTRY OF MINERALS IN FELDSPATHOID- BEARING ROCKS, LOCATED IN NORTH SHAHR-BABAK, WEST MEIDUK VILLAGE

Author(s)

MORADIAN A. | Issue Writer Certificate

Keywords

ALKALINE ROCKSQ3

DIOPSIDEQ3

SANIDINEQ2

PLAGIOCLASEQ1

TITANOMAGNETITEQ3

Abstract

The studied volcanic ALKALINE ROCKS with 32.7±6 Ma years age are croped out along the south - east of Urumiyeh- Dokhtar Volcanic Beltin Kerman province. Based on the TAS classification these rocks are divided in to tephriphonolite and phonolite which belong to high-K ALKALINE ROCKS. These rocks are composed of pyroxene, PLAGIOCLASE, SANIDINE, nepheline, analcime and TITANOMAGNETITE minerals. DIOPSIDE is the only pyroxene identified in the study area. In the most of the phenocrysts the amount of MgO in the core is more than the rims while the amount of FeO is high in the rims. This trend shows a normal fractionation during magmatic evolution. The composition of pyroxene phenocrysts is from WO47.8 En38.8 FS13.4 to WO45.6 En35.7 FS18.8-Sanidine is the only K-feldspar present in these rocks and has a composition ranges from Or62.7to Or93.8 Most of the PLAGIOCLASE phenocrysts have Ca-rich cores and more Na-rich rims which is attributed to normal magmatic fractionation. The composition range of PLAGIOCLASE is An5o.83 to An59.2. Trapezohedrs of analcime comprise up to 40% of the rocks and the composition of the analcime trapezohedrs are remarkably homogeneous. The analcime is interpreted as having formed by ion-exchange pseudomorphous replacement of primary leucite, either during cooling of the lava or shortly afterwards. TITANOMAGNETITE is a very common equant grain in groundmass of all the studied samples. The Fe-Ti oxide crystals are relatively Ti-rich and are classified as titan magnetite.

Cites

No record.

References

No record.

Cite

APA: Copy

MORADIAN, A.. (2006). PETROGRAPHY AND GEOCHEMISTRY OF MINERALS IN FELDSPATHOID- BEARING ROCKS, LOCATED IN NORTH SHAHR-BABAK, WEST MEIDUK VILLAGE. IRANIAN JOURNAL OF CRYSTALLOGRAPHY AND MINERALOGY, 13(2), 215-228. SID. https://sid.ir/paper/4214/en

Vancouver: Copy

MORADIAN A.. PETROGRAPHY AND GEOCHEMISTRY OF MINERALS IN FELDSPATHOID- BEARING ROCKS, LOCATED IN NORTH SHAHR-BABAK, WEST MEIDUK VILLAGE. IRANIAN JOURNAL OF CRYSTALLOGRAPHY AND MINERALOGY[Internet]. 2006;13(2):215-228. Available from: https://sid.ir/paper/4214/en

IEEE: Copy

A. MORADIAN, “PETROGRAPHY AND GEOCHEMISTRY OF MINERALS IN FELDSPATHOID- BEARING ROCKS, LOCATED IN NORTH SHAHR-BABAK, WEST MEIDUK VILLAGE,” IRANIAN JOURNAL OF CRYSTALLOGRAPHY AND MINERALOGY, vol. 13, no. 2, pp. 215–228, 2006, [Online]. Available: https://sid.ir/paper/4214/en

Related Journal Papers