Földrajz színhely Emelő an early diagenetic deglacial origin for basal ediacaran cap dolostones emuláció Tapintat mesterfokozat
PDF) Geochemistry of Ediacaran cap dolostones across the Yangtze Platform, South China: implications for diagenetic modification and seawater chemistry in the aftermath of the Marinoan glaciation
Figure 2 from Are basal Ediacaran (635 Ma) post-glacial “cap dolostones” diachronous? | Semantic Scholar
Karstic features and subsequent barite precipitation in cap dolostones.... | Download Scientific Diagram
Geochronological and geochemical constraints on the origin of highly 13Ccarb-depleted calcite in basal Ediacaran cap carbonate | Geological Magazine | Cambridge Core
Geochronological and geochemical constraints on the origin of highly 13Ccarb-depleted calcite in basal Ediacaran cap carbonate | Geological Magazine | Cambridge Core
The tempo of Ediacaran evolution | Science Advances
Frontiers | New Facies Model and Carbon Isotope Stratigraphy for an Ediacaran Carbonate Platform From South America (Tamengo Formation—Corumbá Group, SW Brazil)
The Marinoan cap carbonate of Svalbard: Syngenetic marine dolomite with 17O‐anomalous carbonate‐associated sulphate - Fairchild - The Depositional Record - Wiley Online Library
Figure 2 from Are basal Ediacaran (635 Ma) post-glacial “cap dolostones” diachronous? | Semantic Scholar
A transient peak in marine sulfate after the 635-Ma snowball Earth | PNAS
A ubiquitous hydrothermal episode recorded in the sheet-crack cements of a Marinoan cap dolostone of South China: Implication for the origin of the extremely 13C-depleted calcite cement - ScienceDirect
CP - Relations - Technical note: Lithium isotopes in dolostone as a palaeo-environmental proxy – an experimental approach
Cryptic terrestrial fungus-like fossils of the early Ediacaran Period | Nature Communications
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Geochemistry of Ediacaran cap dolostones across the Yangtze Platform, South China: implications for diagenetic modification and seawater chemistry in the aftermath of the Marinoan glaciation | Journal of the Geological Society
Figure 2 from Are basal Ediacaran (635 Ma) post-glacial “cap dolostones” diachronous? | Semantic Scholar
The Ediacaran record of glaciogenic dropstones, diamictites and cap carbonates associated with non-metamorphosed banded iron formations (BIFs) in Iran - ScienceDirect
Minerals | Free Full-Text | Chemically Oscillating Reactions during the Diagenetic Formation of Ediacaran Siliceous and Carbonate Botryoids
A-D: Thin-section microphotographs of cap dolostone showing three... | Download Scientific Diagram
An early diagenetic deglacial origin for basal Ediacaran "cap dolostones" | Request PDF
The Marinoan cap carbonate of Svalbard: Syngenetic marine dolomite with 17O‐anomalous carbonate‐associated sulphate - Fairchild - The Depositional Record - Wiley Online Library
Snowball Earth | SpringerLink
Figure 2 from Are basal Ediacaran (635 Ma) post-glacial “cap dolostones” diachronous? | Semantic Scholar
The Ediacaran record of glaciogenic dropstones, diamictites and cap carbonates associated with non-metamorphosed banded iron formations (BIFs) in Iran - ScienceDirect
Chapter 18. The Ediacaran Period
Geochronological and geochemical constraints on the origin of highly 13Ccarb-depleted calcite in basal Ediacaran cap carbonate | Geological Magazine | Cambridge Core
Stratigraphic expression of Earth's deepest δ13C excursion in the Wonoka Formation of South Australia | American Journal of Science