Home

szomorúság Tisztázd Hullámzik an early diagenetic deglacial origin for basal ediacaran cap dolostones Fütykösbot kétkomponensű Kimenő

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

PDF) Geochronological and geochemical constraints on the origin of highly  13 C carb -depleted calcite in basal Ediacaran cap carbonate
PDF) Geochronological and geochemical constraints on the origin of highly 13 C carb -depleted calcite in basal Ediacaran cap carbonate

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)

Open Research Online oro.open.ac.uk
Open Research Online oro.open.ac.uk

SNOWBALL EARTH
SNOWBALL EARTH

PDF) Geochronological and geochemical constraints on the origin of highly  13 C carb -depleted calcite in basal Ediacaran cap carbonate
PDF) Geochronological and geochemical constraints on the origin of highly 13 C carb -depleted calcite in basal Ediacaran cap carbonate

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

Localities of studied cap dolostone sections on the Yangtze Platform.... |  Download Scientific Diagram
Localities of studied cap dolostone sections on the Yangtze Platform.... | 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

Chapter 18. The Ediacaran Period
Chapter 18. The Ediacaran Period

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

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

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 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

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

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

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

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

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