Geochemistry of Asara Shale member of Karaj Formation, Central Alborz, Iran: Provenance, source weathering and tectonic setting
Autor: | Salvatore Critelli, Mohammad Malekzadeh, Abbas Sadeghi, Mahboubeh Hosseini-Barzi |
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Rok vydání: | 2020 |
Předmět: |
Provenance
010504 meteorology & atmospheric sciences Stratigraphy Continental crust Geochemistry Geology engineering.material 010502 geochemistry & geophysics Oceanography 01 natural sciences Sedimentary depositional environment Geophysics Continental margin Clastic rock Illite engineering Economic Geology Siliciclastic Oil shale 0105 earth and related environmental sciences |
Zdroj: | Marine and Petroleum Geology. 121:104584 |
ISSN: | 0264-8172 |
Popis: | The Asara Shale Member of the Karaj Formation, Middle to Upper Eocene in age, includes mixed volcaniclastic, siliciclastic and carbonate strata, in the Alborz Mountains, northern Iran. These strata have been geochemically analyzed to constrain their source area provenance. Most of the major and trace element contents of Asara Shale samples are generally similar to the upper continental crust (UCC) values and their chemical index of alteration (CIA) values (31.7–50.9), suggesting a semi-arid climate in a weathering-limited source area. Moreover, correlation of major element oxides suggests the controlling effect of plagioclase and clay minerals on these data when XRD analysis and SEM images indicate clastic sourced illite and chlorite in the samples, probably due to the weathering of volcanic ash and glass in an aqueous transport and depositional environment. However, the chondrite-normalized REE plot of mudrocks of the Asara Shale show a similarity with the UCC composition. Mineral composition and geochemistry of the Asara Shale mudrocks reveal the rapid reworking of penecontemporaneous volcaniclastic deposits, which had covered the surrounding areas, instead of their epiclastic genesis related to erosion and transport. Major, trace, and rare earth element (REE) data, imply a felsic composition of the volcanic source, related to an active continental margin/continental island arc and most probably back-arc tectonic setting for the depositional basin, inferring a mid-upper Eocene extensional volcanism in a subduction complex. |
Databáze: | OpenAIRE |
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