The Influence of Petrography on the Relief of Bistriţei Mountains (The Eastern Carpathians) by Iulian SĂNDULACHE, Cătălina SĂNDULACHE, Alexandra RIZAC, Mihaela RAȘCU

“…In the south, slender hills appear, due to the presence of dolomites and limestones, whose hardness exceeds that of the metamorphic rocks surrounding them. …”
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Structure and formation of the Lower Cretaceous–Eocene section in the central part of the Simferopol Uplift by K.A. Dubkova, S.B. Shishlov, E.M. Bugrova, E.Yu. Zakrevskaya

“…Sandy marls with boulders of nummulitic limestones lie above, they must have formed in highly dynamic shallow marine conditions. …”
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Hydrogeology and Hydrogeochemistry of the Lauria Mountains Northern Sector Groundwater Resources (Basilicata, Italy) by Filomena Canora, Giovanna Rizzo, Simona Panariello, Francesco Sdao

“…The analyses highlight that the chemical compositions of groundwater are strongly influenced by the lithology, especially limestones and dolomitic limestones; they explain and confirm the hydrogeological setting of the system. …”
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Facies distribution, sequence stratigraphy, and reservoir quality of the Oligo-Miocene carbonate sequences (Asmari formation) in the Dezful embayment, SW Iran by Hamed Sadeqi, Mohsen Aleali, Ali Kadkhodaie, Mehran Arian

“…This succession in the Haft-Kel Field contains limestones, dolostones, anhydrites, and argillaceous limestones and is bounded between the Pabdeh and Gachsaran formations. …”
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PT-FORMATION CONDITIONS OF POLYMETALLIC ORES FROM THE Pb-Zn-Fe AKTASH SKARN DEPOSIT (WESTERN KARAMAZAR, TAJIKISTAN) by U.A. Yatimov, N.N. Ankusheva, M.A. Rassomakhin

“…The deposit is confined to a contact zone between carbonate (Upper Devonian–Lower Carboniferous dolomite and limestones) and intrusive rocks (Middle Carboniferous–Early Triassic granodiorites and porphyry granodiorites) of the Kansai ore field. …”
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The Neolithic layer of the Maryeva Gora archaeological complex near the village of Kulbakovo, Rostov region: materials for the Collection of sites by Manko N.V., Danilchenko A.Yu.

“…Limestones, marls and chalk of the Upper Cretaceous age are massively exposed on the slopes of rivers and gullies within the Southern Donbass. …”
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Investigation of the Effects of Marble Material Properties on the Surface Quality by Sümeyra Cevheroğlu Çıra, Ahmet Dağ, Askeri Karakuş

“…For this purpose, four types of limestones were investigated. Physicomechanical properties of samples were determined through laboratory measurements. …”
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From Middle Jurassic extension to Late Jurassic obduction: sedimentary records from the Greater Adriatic margin of the Neotethys Ocean in NE Hungary by Szilvia Kövér, János Haas, Nevenka Djerić, Ottilia Szives, Péter Ozsvárt, László Fodor

“…The sedimentation in its Bajocian–early Callovian extensional half-grabens was characterised by pelagic limestones followed by dark shales with sandstone intercalations. …”
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Middle to Late Jurassic pelagites and gravity mass flow deposits of a displaced Neotethyan margin: Microfacies and biostratigraphical studies in Northeast Hungary by Haas János, Fodor László, Đerić Nevenka, Szives Ottilia, Ozsvárt Péter, Fialowski Melinda, Kövér Szilvia

“…The Recsk Succession is made up of Upper Triassic, cherty carbonates of pelagic basin development that are overlain by pelagic limestones of Early to early Middle Jurassic age. The carbonate sedimentation changed gradually into shale‐domi nated one during the late Bathonian to the early Callovian. …”
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Detailed Fluid Inclusion and Stable Isotope Analysis on Deep Carbonates from the North Alpine Foreland Basin to Constrain Paleofluid Evolution by Elena Mraz, Markus Wolfgramm, Inga Moeck, Kurosch Thuro

“…Salinity and formation temperature of paleofluids in fluid inclusions and isotope data are consistent with previous studies and reveal a 5-stage evolution: the main cementation phases are composed of (I) the early diagenesis in limestones (200-400 m, 40-50°C), (II) early diagenetic dolomitization, and (III) burial dolomitization (1-2 km, II: 40-90°C; III: 70-100°C; 40 g/L NaCl equiv.), and (IV) late burial calcification (IIIa: 110-140°C, IIIb: 140-200°C) linked to tectonic features in the Molasse Basin. …”
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