Zur Geologie des Kelkit Çay-Oberlaufs Südwestlich von Şiran (Nordostanatolien)
The region situated east of Berdiga Dağ is built up by Mesozoic and Tertiary Sediments. The Mesozoic sequence begins with Lias and ends with Upper Cretaceous. During the Laramic orogenetic phase this sequence was folded with E-W striking axes.
Karl NEBERT
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The deep origin of ground fissures in the Kenya Rift Valley. [PDF]
Jia Z +8 more
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Study on the Source Contributions of Gas Reservoirs in the Dongfang and Ledong Areas of the Yinggehai Basin. [PDF]
Pei J +5 more
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Quaternary to recent uplift rates of salt diapirs in the Romanian Carpathians determined from radiocarbon dating and PSInSAR data. [PDF]
Tamas DM +5 more
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Arc magma formation through the fluid-fluxed mélange melting in subduction zones. [PDF]
Zhang W +4 more
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Fungal Diversity and Composition of the Continental Solar Saltern in Añana Salt Valley (Spain). [PDF]
Azpiazu-Muniozguren M +9 more
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Microbial and geochemical architecture of an active Scotian Slope cold seep. [PDF]
Redshaw E +12 more
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Cold seep formation from salt diapir-controlled deep biosphere oases. [PDF]
Chowdhury A +13 more
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Helium isotope anomaly in groundwater prior to the 2024 Noto Peninsula earthquake. [PDF]
Kagoshima T +8 more
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Petrogenesis of juvenile pelletal lapilli in ultramafic lamprophyres. [PDF]
Prokopyev I +5 more
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