Results 31 to 40 of about 1,105,251 (141)
Geological and geophysical survey in the Bellingshausen Basin, off Antarctica
Antarctic Record, 1982 The continental margin in the Bellingshausen Basin off West Antarctica was geologically and geophysically surveyed. The paleo-trench, which has been inferred from the seafloor magnetic anomalies, is found out in the 3-fold seismic reflection profiles. In
Katsuhiro Kimura
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Geological properties of Güney formation (Ereğli - Ulukışla Basin, Niğde)
Bulletin of the Mineral Research and Exploration, 2021 The aim of this study to determine stratigraphic, sedimentological and petrographic characteristics of the Upper Paleocene - Lower Eocene Güney formation in the Ereğli - Ulukışla Basin based on the lithological and environmental interpretations related ...
Nurettin Sonel, Ayfer Özdemir
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The Araxá Group in the South-Southwest Region of the Goiás State [PDF]
Geologia USP. Série Científica, 2013 In the S – SW region of Goiás State, Brazil, the Araxá Group is constituted of a metasedimentary sequence containing schistoseand gneissic (garnet-biotite-quartz schists, feldspatic garnet-biotite-quartz schists, garnet-biotite-quartz paragneisses,with ...
Guillermo Rafael Beltran Navarro +2 more
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Heliyon, 2018 The purpose of this study is to reexamine the age, depositional environment, and tectonic setting of the Tsunemori Formation. This study provides a new tectonic model on the formation of Tsunemori Formation, which is a key formation to understand the ...
Koji Wakita, Ruri Yoshida, Yuki Fushimi
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Seismic Velocity Structure Beneath the Tofino Forearc Basin Using Full Waveform Inversion
Energies, 2021 Given the effects of steep dips and large lateral variations in seismic velocity beneath the Vancouver Island continental shelf, seismic processing and travel time inversion are inadequate to obtain a detailed velocity model of the subsurface. Therefore,
Subbarao Yelisetti, George D. Spence
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Geologica Acta, 2023 The mantle rocks from Kadaboura and Madara areas represent sections of dismembered ophiolitic complexes developed during the Neoproterozoic in the Eastern Desert of Egypt, which is located in the northwestern corner of the Arabian–Nubian Shield.
Shehata Ali +2 more
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Geophysical Research Letters, 2012 We have investigated how an arc‐ward increase in bulk mechanical strength in an experimental accretionary prism influences the development, timing, and duration of slip on out‐of‐sequence thrusts.
Saad S. B. Haq
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Indonesian Journal on Geoscience, 2014 http://dx.doi.org/10.17014/ijog.vol4no1.20095The Tertiary Bengkulu Basin is known as a typical fore-arc basin, situated in southwest Sumatera. The basin initiated during Eocene-Oligocene times, accumulates the Lahat equivalent formation. The formation is
Hermes Panggabean, R. Heryanto
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Geological Journal, EarlyView.Coupled dissolution‐reprecipitation of early formed Cd‐, Fe‐, Ag‐ and Sb‐poor sphalerite through interaction with high‐temperature and high‐sulphur fugacity Cu‐rich fluids, responsible for the formation of the yellow ores, resulted in the formation of Cd‐, Fe‐, Ag‐ and Sb‐rich, heavily chalcopyrite‐diseased sphalerite and enrichment of critical metals ...
Manuel Nopeia +4 more
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Geological Journal, EarlyView.The composition of intrusive rocks suggests that the magma was likely generated in a subduction‐related setting. The arc crustal thickness in the Phnom Sro Ngam and Halo Prospects was probably < 40 km during emplacement. Zircon U–Pb age range indicates a correlation with Loei Fold Belt magmatic activity.
Sirisokha Seang +6 more
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