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Petrology, Geochemistry and Tectonomagmatic Evolution of Hezar Igneous Complex (Rayen- South of Kerman- Iran): the First Description of an Arc Remnant of the Neotethyan Subduction Zone

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Academic year: 2020

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Figure

Figure 1. The approximate location of the study area on tectonic map of Iran [2] and 1/100.000 geological map of Rayen.
Figure 2. (a) Nonwelded tuff with a tent structure or sugarloaf structure; (b) Three different structures in pyroclastic rocks; alayer of welded tuff is located between two volcanic surge deposits
Figure 3. Some microphotographs of different rock types in HIC: a) A decomposing amphibole crystal in an andesitic basalt; b)Flow texture in a pyroclastic rock whose pores filled with secondary products such as calcite; c) Rhyolite with columnar structurei
Table 1. Geochemical analysis of 28 rock samples using ICP-MS and XRF with calculated CIPW normative minerals.
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