Возраст питающих провинций Горловского передового прогиба: результаты датирования детритовых цирконов из песчаников балахонской серии

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Геосферные исследования. 2017; : 33-48

Возраст питающих провинций Горловского передового прогиба: результаты датирования детритовых цирконов из песчаников балахонской серии

Жимулев Ф. И., Гиллеспи Д. , Глорие С. , Ветров Е. В., Борискина В. И., Караковский Е. А., Де Г. Й.

https://doi.org/10.17223/25421379/3/3

Аннотация

В результате U/Pb LA-ICP-MS датирования детритовых цирконов из пермских песчаников балахонской серии в Горловском передовом прогибе были выявлены следующие возрастные популяции цирконов: неопротерозойская (840-710 млн лет, 14%), кембрийско-раннеордовикская (530-460 млн лет с максимумом на 498 млн лет, 28%) и каменноугольно-пермская (380-280 млн лет c максимумом на 322 млн лет, 50%).

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Geosphere Research. 2017; : 33-48

The age of the source provenance of the Gorlovo foreland basin: detrital zircon U/Pb ages of balakhon group sandstones

Zhimulev F. I., Gillespie J. A., Glorie S. , Vetrov E. V., Boriskina V. I., Karakovskiy E. A., De G. J.

https://doi.org/10.17223/25421379/3/3

Abstract

The aim of this paper is determination the sources provinces and paleotectonic environments of the Gorlovo coal-bearing basin, located in the junction zone between Caledonian and Hercynian fold systems of the Altay-Sayan folded area. The Caledonian structures of this region are represented by the Salair terrane, and the Hercynian structures are represented by the Kolyvan-Tomsk folded zones (KTFZ). The structural position, morphology, composition of sedimentary cover and the internal structure, indicates that the Gorlovo basin is a foreland basin. The tectonic evolution of the Gorlovo Basin is the result of the late Paleozoic collision processes, which led to the formation of the nappe structure of the KTFZ. The KTFZ is considered as an external, part of a larger Central-West Siberian fold system. The inner regions of Central-West Siberian fold system are hidden by the West Siberian Basin cover. The sedimentary section of the Gorlovo basin includes two main units: - Late Devonian- Visean carbonate-terrigenous deposition, comparable with the same age deposits at the KTFZ and Salair region and terrigenous molasses covering interval Serpukhovian - Permian. The last unit has no analogs in the adjacent tectonic zones. The lower part of the molasses, the elbashin formation, accumulated in marine environments, the upper part, including the Balakhon and Kolchugin Groups, was formed under continental environments. Dating of detrital zircons from alluvial sandstones of the Upper Carboniferous-Lower Permian Balakhon Group are presented in the paper. 84 zircon grains were dated. 78 grains from them have discordance less than 10%, only these were used to construct diagrams of the relative probability of ages. Diagrams of the relative probability of ages (age spectra) for the analyzed samples were plotted at²⁰⁶Pb /²³⁸U for grains less than 1 billion years old and²⁰⁷Pb /²⁰⁶Pb for grains older than 1 billion years. The age range of sample 15-471 comprises three significant age population - Neoproterozoic (840-710 Ma without contrast maximum) Cambrian-Early Ordovician (530460 Ma with a maximum at 498 Ma) and Carboniferous-Permian (380-280 Ma with a maximum at the 322 Ma). Neoproterozoic zircons represent 14% of concordant values, early Paleozoic - 28%, late Paleozoic -50%, and 5% accounted for the ancient zircons with ages 2.7-1.8 billion years. The oldest grain has an age of 2718 Ma, the youngest - 282 Ma. At the CL-images Paleozoic zircons are clearly oscillatory zoning whereas in the Neoproterozoic population nonzonal grains with a uniform or bloc internal structure are occur. Paleozoic zircons, usually are represented by euhedral grains, the grains of Precambrian zircons are often well-rounded. Th / U ratio for all grains lies in the range of 0.2-1.56, averaging 0.73. There are no regular changes in the Th / U ratio in different populations are observed. The neodymium model age TNd (DM)of the studied sandstone is 1066 Ma, the age calculated from the two-stage model of TNd (DM-2st) = 1174 Ma, sNd (T) = -1.33. There are no any magmatic events were distinguished in this time at the study area. Zircons with similar ages are absent in the sandstone sample. So, model age can reflect the mixing of the relatively young juvenile crust, which could be the early Paleozoic deposits from Salair, with a small contribution of the ancient source which could be Siberian craton. Relatively high for enough mature continental sediment, the value of sNd (T) indicates that juvenile Paleozoic magmatic complexes were the main source for sediments, and contribution of the ancient continental crust was of the rocks was subordinate. Our data confirm the absence in the basement of Salair terrane any ancient continental crust. Magmatic activity in the source province, lasted a very narrow range of 550-460 Ma, and majority of zircons have ages of 510-480 Ma. The last interval can be interpreted as a time of the main magmatic activity on the Salair and corresponds to the volcanic Green- Purple Group forming. There are gap on the age spectrum between the early Paleozoic and late Paleozoic peaks. This gap lasted from 450 to 380 Ma (late Ordovician - Early Devonian). The age of 380 Ma, corresponds to the beginning of the bimodal volcanism of the Bugotak complex, which forms the base of the KTFZ. An empty interval in the age spectrum of detrital zircons corresponds to the major break in the sedimentary section of region. In the Late Ordovician - Early Devonian northern Salair was in the subplatform tectonic regime. The largest number of zircons (50%) has late Paleozoic age (380-282 Ma), most of the ages are lie within the range of 350-300 Ma. Most of the zircons have ages very close to the time of accumulation of the Balakhon Group. This fact can be explained by the brining of zircon from volcanic deposits of the Carboniferous age, as well as the high rate of exhumation of granite inrtusions in the source province. Late Devonian-Carboniferous volcanic rocks are absent at the KTFZ and Salair zones, but are widely developed in the axial part of the Ob-Zaisan fold system, its complexes are exposed in East Kazakhstan and Rudny Altai and follow in the basement of the West Siberian plate to the west and northwest of KTFZ. Thus, in the early Permian time, the sediment supply into the Gorlovo Basin occurred predominantly from the northwest, from the growing orogen, composed of magmatic complexes of the accreted Carboniferous island arc. These data confirm the interpretation of the Gorlovo Basin in the late Carboniferous - Permian, as a foreland basin.

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Возраст питающих провинций Горловского передового прогиба: результаты датирования детритовых цирконов из песчаников балахонской серии

Аннотация

The age of the source provenance of the Gorlovo foreland basin: detrital zircon U/Pb ages of balakhon group sandstones

Abstract

События