جستجوی مقالات مرتبط با کلیدواژه « parent rock » در نشریات گروه « علوم پایه »

In this study, a combination of petrographic and major element geochemistry of siliciclastic deposits of Lower Permian Doroud Formation in the Zal section in south of Jolfa has been used to investigate the provenance, tectonic setting and paleo-weathering. The thickness of Doroud Formation in Zal section is 112 m consisting of micro conglomerate, red sandstone and shale. Thirteen samples of sorted and medium grained sandstones were examined by point-counting method and 6 samples were examined for determination of their major elements by X-ray fluorescence (XRF) method. The studied samples are frequently sublithic-arenite in composition. The study of the amount and type of monocrystalline and polycrystalline quartz and using of discrimination function, indicate that the parent rocks of these deposits are predominantly metamorphic, felsic igneous rocks as well as sedimentary recycled. The presence of chert in petrographic studies has also confirmed the effect of sedimentary recycling from older formations. Petrographic and geochemical studies also indicate the cratonic origin and tectonic setting of the passive continental margin at the time of sediment deposition of the Doroud Formation. Determination of chemical index of alteration (CIA) indicates intense weathering and humid climate in the provenance area, which is consistent with the paleogeography of the Iran in Permian. It seems that factors such as the a long-distance transport on the Arabian Craton, the recycling of older formations and also the humid climate at the time of the deposition of the Doroud Formation, together, have played significant role at the relatively high maturity of this sandstones.

 In this study, petrography and geochemistry of the sandstones and shales of Padeha Formation in Khoshyeilagh section in Eastern Alborz have been used to obtain more information on their provenance. The Padeha Formation in the studied section has a thickness of 341 meters and overlies the Late Ordovician-Silurian Soltan-Meydan basalts and disconformably underlies the Middle to Upper Devonian Khoshyeilagh Formation. After field studies, 20 medium-grained sandstone samples were selected for point-counting and eight sandstone and two shale samples were selected for geochemical analysis. Based on the calculated percentages of point counting data, the composition of these sandstones has been detected as quartzarenites, subarkose and sub litharenites. Based on Q/Q+F in sandstones and geochemical properties of sandstones and shales, such as Al2O3/TiO2 ratio and TiO2 against Zr, the dominant parent rock of these deposits can be considered as felsic igneous rocks. The QmFLt and QtFL diagrams show the tectonic setting of the Padeha sandstones as a stable craton. The geochemistry has also largely confirmed the tectonic setting of passive continental and rifted margins. Considering paleogeography of the region, tectonic uplifts and erosion of the Cadomian granitic basement and also the entrance of clastic materials from granitic rocks of Arabian craton can be considered as other source rocks of the sediments of Padeha Formation.

     Petrography and the composition of siliciclastic sediment and sedimentary rock components provide important information on parent rock, which is one of the main factors in the reconstruction of tectonic evolution and sedimentation. In addition, by using the chemical composition (major, trace and rare earth elements) of siliciclastic sediments and sedimentary rocks, one can also estimate the provenance and other sedimentary processes such as weathering, transport and diagenesis (McLennan et al. 1993; Armstrong-Altrin et al. 2012; Armstrong-Altrin 2015).
In this study, petrography and geochemistry of the sandstones and shales of the Padeha Formation in Khoshyeilagh section in Eastern Alborz have been used to obtain more information on their provenance.
 

     The Padeha Formation in the studied section has a thickness of 341 meters and overlies the Late Ordovician-Silurian Soltan-Meydan basalts and disconformably underlies the Middle to Upper Devonian Khoshyeilagh Formation. In this study, 30 samples of sandstones of the Padeha Formation in Khoshyeilagh section were selected after field sampling and petrographic studies. Twenty medium- to fine-grained sandstone samples were selected for modal analysis, and about 300 points were counted on every thin section using the Gazzi-Dickinson method (Ingersoll et al. 1984). According to the point counting, the main and accessory components of this sandstones are identified and quartz, feldspar and rock fragments modes are utilized for naming the sandstones according to the Folk classification (Folk 1980) as well as different diagrams of the provenance (Dickinson 1985). Based on the calculated percentages of point counting data, the composition of these sandstones has been detected as quartz arenites, sub arkose and sub litharenites. Eight samples of medium-grained sandstone samples with the lowest amount of carbonate cement and two samples of shales in the middle member of the Padeha Formation were selected, crushed and powdered with a mill and sent to the Zarazma Laboratory, Tehran for geochemical analysis (ICP-MS method) to determine the major, trace and rare earth elements.
 

    According to the ratio of quartz to total feldspar and quartz in the sandstones of the Padeha Formation, which is 0.95 and geochemical properties of sandstones and shales, such as Al2O3/TiO2 ratio and TiO2 against Zr, the dominant parent rock of these deposits can be considered as felsic igneous rocks. The QmFLt and QtFL diagrams show the tectonic setting of the Padeha sandstones as a stable craton. Passive continental and rifted margins for Padeha Formation has also largely confirmed by geochemistry of sandstone and shale samples. Considering paleogeography of the region, tectonic uplifts and erosion of the Cadomian granitic basement and also the entrance of clastic materials from granitic rocks of Arabian craton can be considered as the other source rocks of the sediments of Padeha Formation.

In this study, petrological and geochemical characterizes of major elements of the Dahu Formation sandstones (lower Cambrian) in Abyaneh section which in west of Natanz, Central Iran have been investigated to specify the origin, tectonic setting and paleoweathering condition. According to petrological studies, sandstones in this region are fine to coarse grained with intermediate to good sorting. Generally these sandstones are identified as litharenite, sub-litharenite, quartz-arenite and partially pheldesphtic litharenite. By comparing major elements with UCC shows that all elements (except CaO and MnO) have depleted with respect to upper continental crust (UCC). Geochemical data in tectonic setting discernment diagrams show that sandstones were deposited in active continental margin mainly. High value (93) of chemical weathering index (CWI) suggests an intermediate igneous source rocks with wet and warm condition.