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  1. 61

    A Review of Research Progress on Re-Os Isotopic System of Carbon-enriched Geological Samples by LI Xinwei, LI Chao, ZHOU Limin, ZHAO Hong, QU Wenjun

    Published 2023-03-01
    “…The coupling relationship between the variation of Os isotopic ratios, atmospheric oxygen level, crustal weathering degree, glaciation events, meteorite impact events, and Large Igneous Provinces can provide the occurrence time and explore the mechanism of major geological events in the history of the earth. The paleoseawater environment and paleoclimate during sedimentation can be further reduced in multiple dimensions by means of the coordinated variation between Re-Os isotopic data, organic matter accumulation, enrichment degree of redox-sensitive elements, and other geochemical proxies.The behavior of Re and Os in the oil-gas system has always been the focus and difficulty in the research of oil-gas reservoir chronology, which is an important basis for understanding the geological significance and wide application of oil-gas reservoir-related samples. …”
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  2. 62

    National and messianic themes in the iconography of St John of Dukla. A case study of the hagiographic cycle by Tadeusz Sulima Popiel in Dukla by Cyprian Janusz Moryc

    Published 2016-06-01
    “…The national and Messianic elements that linked the life of St John and the history of his earthly homeland to the history of the Chosen People already figured centrally in the early iconography of the saint, with its most emblematic image of the Defensor Leopolis, but became even more widespread in the 19th and 20th centuries. …”
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  3. 63

    A prolonged granitoid formation in Saglek Block, Labrador: Zonal growth and crustal reworking of continental crust in the Eoarchean by Tsuyoshi Komiya, Shinji Yamamoto, Shogo Aoki, Keiko Koshida, Masanori Shimojo, Yusuke Sawaki, Kazumasa Aoki, Shuhei Sakata, Takaomi D. Yokoyama, Kenshi Maki, Akira Ishikawa, Takafumi Hirata, Kenneth D. Collerson

    Published 2017-03-01
    “…The Archean continental crusts account for ca. 20% of the present volume, but the thermal history of the Earths' mantle suggests much more continental crusts were formed in the early Archean. …”
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