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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
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
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
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

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
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)
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
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
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 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
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
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
Cryptic terrestrial fungus-like fossils of the early Ediacaran Period | Nature Communications

Research Projects
Research Projects

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
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
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
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
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
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
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
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
Snowball Earth | SpringerLink

Figure 2 from Are basal Ediacaran (635 Ma) post-glacial “cap dolostones”  diachronous? | Semantic Scholar
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
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
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
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
Stratigraphic expression of Earth's deepest δ13C excursion in the Wonoka Formation of South Australia | American Journal of Science