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NARROW
GeoRef Subject
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all geography including DSDP/ODP Sites and Legs
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Europe
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Central Europe
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Germany (1)
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Southern Europe
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Iberian Peninsula
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Spain
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Andalusia Spain
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Almeria Spain (1)
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Italy
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Emilia-Romagna Italy
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Ravenna Italy (1)
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Piemonte Italy
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Asti Italy (1)
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elements, isotopes
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isotope ratios (1)
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isotopes
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stable isotopes
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O-18/O-16 (1)
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S-34/S-32 (1)
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Sr-87/Sr-86 (1)
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metals
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alkaline earth metals
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strontium
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Sr-87/Sr-86 (1)
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oxygen
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O-18/O-16 (1)
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sulfur
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S-34/S-32 (1)
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fossils
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microfossils (1)
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Plantae
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algae
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diatoms (1)
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geologic age
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Cenozoic
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Tertiary
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Neogene
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Miocene
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upper Miocene
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Messinian (2)
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Mesozoic
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Triassic
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Upper Triassic
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Keuper (1)
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minerals
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selenites (1)
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sulfates
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gypsum (2)
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Primary terms
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Cenozoic
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Tertiary
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Neogene
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Miocene
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upper Miocene
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Messinian (2)
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crystal growth (1)
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Europe
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Central Europe
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Germany (1)
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Southern Europe
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Iberian Peninsula
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Spain
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Andalusia Spain
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Almeria Spain (1)
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Italy
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Emilia-Romagna Italy
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Ravenna Italy (1)
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Piemonte Italy
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Asti Italy (1)
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geochemistry (1)
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inclusions
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fluid inclusions (1)
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isotopes
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stable isotopes
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O-18/O-16 (1)
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S-34/S-32 (1)
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Sr-87/Sr-86 (1)
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Mesozoic
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Triassic
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Upper Triassic
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Keuper (1)
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metals
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alkaline earth metals
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strontium
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Sr-87/Sr-86 (1)
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oxygen
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O-18/O-16 (1)
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paleoecology (1)
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Plantae
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algae
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diatoms (1)
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sea water (1)
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sedimentary rocks
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chemically precipitated rocks
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evaporites
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salt (1)
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clastic rocks
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mudstone (1)
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sediments
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marine sediments (1)
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sulfur
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S-34/S-32 (1)
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sedimentary rocks
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sedimentary rocks
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chemically precipitated rocks
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evaporites
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salt (1)
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clastic rocks
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mudstone (1)
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sediments
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sediments
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marine sediments (1)
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Yesares Selenites
Sr, S, and O isotope data of the Yesares selenites and vein gypsum.
A) 87 Sr/ 86 Sr vs. Sr concentration for Nijar Yesares selenites. The dash...
A) δ 34 S vs δ 18 O SO 4 of the Yesares selenites. The box represents δ ...
Sr, S, and O SO 4 Isotopes and the Depositional Environments of the Upper Miocene Evaporites, Spain
Coarse-crystalline selenites and their vertical growth fabrics in the Yesar...
Tiny, glassy, and rapidly trapped: The nano-sized planktic diatoms in Messinian (late Miocene) gypsum
Are fluid inclusions in gypsum reliable paleoenvironmental indicators? An assessment of the evidence from the Messinian evaporites
Saltern, mudflat, and dry playa: playa basin types of a retreating epeiric sea (Keuper, Germany)
Abstract The Carboneras Fault Zone (CFZ) of SE Spain separates the volcanic Cabo de Gata terrain to the SE (accumulated over 18 to 6 Ma BP) from the tract of uplifted Alpine metamorphic basement blocks and post-orogenic basins that comprise the Betic Cordilleras to the NW. The CFZ cuts metamorphic basement and folded post-orogenic sediments and volcanic rocks, and acted as a conduit for upper Miocene calc-alkaline volcanic rocks to the surface. NW of the CFZ, unconformities and deformation episodes affect successive sedimentary formations of upper Miocene age (upper Serravallian through Messinian). CFZ movements are constrained stratigraphically by an unconformity within the volcanic sequence. Older, pre-faulting volcanic rocks are uptilted against the CFZ whilst the youngest volcanic rocks step across it. 40 Ar– 39 Ar age determinations on amphibole crysts from the volcanic rocks show the main CFZ movements began 11–12 Ma BP and ended about 6 Ma. Lesser movement rates continue today. The CFZ is interpreted as part of a transform fault system separating NE–SW stretched and NW–SE shortened crust deformed above a southwestward-retreating subducted slab, from a less deformed terrain lying to the SE. Locally, total offset on the CFZ may be up to 40 km but is at least 15 km.