Geochemical compositions can be used to determine the tectonic setting of sedimentary basins,while where the link of source to sink is no longer preserved,detrital zircon age patterns can aid in resolving the original...Geochemical compositions can be used to determine the tectonic setting of sedimentary basins,while where the link of source to sink is no longer preserved,detrital zircon age patterns can aid in resolving the original basin setting.The metasedimentary Legoupil Formation,located at Cape Legoupil and the Schmidt Peninsula,could give a hint for the tectonic evolution of Antarctic Peninsula.In this contribution,we constrain the sedimentary provenance of the Legoupil Formation through geochemistry and detrital zircon U-Pb geochronology.The petrography and geochemical features indicate that the provenance of the Legoupil Formation could be felsic rocks.Detrital zircon grains record a steady supply of Permian and Ordovician material into the Legoupil Formation.The youngest concordant zircon ages of 262 Ma suggest that the depositional time of Legoupil Formation is no older than Late Permian.The detrital zircon age spectrum of Legoupil Formation suggests that the Legoupil Formation sediments should be derived from regional sources endemic to western Gondwana prior to its breakup.Together with the previous studies,geochemistry and detrital zircons reflect an active continental margin tectonic setting and the detrital zircon spectra of Legoupil Formation are similar to the ones deposited in forearc tectonic setting.展开更多
The work is devoted to a problem of seismic activity of northern part of Sakhalin Island.The active faults were trenched and studied in detail.Its expressiveness in a relief and character of displacement of strata is ...The work is devoted to a problem of seismic activity of northern part of Sakhalin Island.The active faults were trenched and studied in detail.Its expressiveness in a relief and character of displacement of strata is discussed.We provide cogent evidences that young tectonic faults on Schmidt peninsula were formed as a result of sharp periodic motions with amplitudes up to several meters and are connected with strong earthquakes.The urgency of work is that there are works on search of hydrocarbons展开更多
基金financially co-supported by the National Natural Science Foundation of China(Nos.41530209,41802238)the Chinese Polar Environment Comprehensive Investigation&Assessment Programs(Nos.CHINARE 2015-02-05,CHINARE 2017-04-03)+1 种基金the Young Scientists Fund of Shandong Province(No.ZR2019PD010)the Opening Foundation of Key Laboratory of Mineral Resources Evaluation in Northeast Asia,Ministry of Land and Resources(No.DBY-KF-19-15).
文摘Geochemical compositions can be used to determine the tectonic setting of sedimentary basins,while where the link of source to sink is no longer preserved,detrital zircon age patterns can aid in resolving the original basin setting.The metasedimentary Legoupil Formation,located at Cape Legoupil and the Schmidt Peninsula,could give a hint for the tectonic evolution of Antarctic Peninsula.In this contribution,we constrain the sedimentary provenance of the Legoupil Formation through geochemistry and detrital zircon U-Pb geochronology.The petrography and geochemical features indicate that the provenance of the Legoupil Formation could be felsic rocks.Detrital zircon grains record a steady supply of Permian and Ordovician material into the Legoupil Formation.The youngest concordant zircon ages of 262 Ma suggest that the depositional time of Legoupil Formation is no older than Late Permian.The detrital zircon age spectrum of Legoupil Formation suggests that the Legoupil Formation sediments should be derived from regional sources endemic to western Gondwana prior to its breakup.Together with the previous studies,geochemistry and detrital zircons reflect an active continental margin tectonic setting and the detrital zircon spectra of Legoupil Formation are similar to the ones deposited in forearc tectonic setting.
文摘The work is devoted to a problem of seismic activity of northern part of Sakhalin Island.The active faults were trenched and studied in detail.Its expressiveness in a relief and character of displacement of strata is discussed.We provide cogent evidences that young tectonic faults on Schmidt peninsula were formed as a result of sharp periodic motions with amplitudes up to several meters and are connected with strong earthquakes.The urgency of work is that there are works on search of hydrocarbons
