STUDY OF DIORITIC INTRUSION AND PYROXENITIC AND ANDESITIC XENOLITHS FROM SW OF SORKH SHAD (NE OF ISFAHAN PROVINCE)

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TORABI GH.A.

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Journal: RESEARCH JOURNAL OF UNIVERSITY OF ISFAHAN "SCIENCE" Year:2006 | Volume:25 | Issue:3 Page(s): 99-116

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Title

STUDY OF DIORITIC INTRUSION AND PYROXENITIC AND ANDESITIC XENOLITHS FROM SW OF SORKH SHAD (NE OF ISFAHAN PROVINCE)

Author(s)

TORABI GH.A. | Issue Writer Certificate

Keywords

DIORITIC IINTRUSIONQ3

XENOLITHQ3

EOCENE VOLCANIC ROCKSQ3

PYROXENITEQ3

Abstract

There are outcrops of Lower-Oligocene dioritic intrusions in south west of Sorkh Shad (NE of Isfahan province). One of these intrusions that are near to Chah Senjed and Chah Ghandehari, has many andesitic and pyroxenitic XENOLITHs. Studies conclude that these XENOLITHs are separated from wall rock during the melt ascending and carried to upper parts. Because of similar composition of andesitic XENOLITHs and ascending dioritic melt, the andesitic XENOLITHs are intact but a chemical potential gradient was established between the dioritic melt and ultrabasic XENOLITHs and calcium and aluminum added to XENOLITHs for new minerals and PYROXENITE formation. The possible temperature of PYROXENITEs formation was 790 to 850 oC.

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APA: Copy

TORABI, GH.A.. (2006). STUDY OF DIORITIC INTRUSION AND PYROXENITIC AND ANDESITIC XENOLITHS FROM SW OF SORKH SHAD (NE OF ISFAHAN PROVINCE). RESEARCH JOURNAL OF UNIVERSITY OF ISFAHAN "SCIENCE", 25(3), 99-116. SID. https://sid.ir/paper/55889/en

Vancouver: Copy

TORABI GH.A.. STUDY OF DIORITIC INTRUSION AND PYROXENITIC AND ANDESITIC XENOLITHS FROM SW OF SORKH SHAD (NE OF ISFAHAN PROVINCE). RESEARCH JOURNAL OF UNIVERSITY OF ISFAHAN "SCIENCE"[Internet]. 2006;25(3):99-116. Available from: https://sid.ir/paper/55889/en

IEEE: Copy

GH.A. TORABI, “STUDY OF DIORITIC INTRUSION AND PYROXENITIC AND ANDESITIC XENOLITHS FROM SW OF SORKH SHAD (NE OF ISFAHAN PROVINCE),” RESEARCH JOURNAL OF UNIVERSITY OF ISFAHAN "SCIENCE", vol. 25, no. 3, pp. 99–116, 2006, [Online]. Available: https://sid.ir/paper/55889/en

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