Oolitic ironstones, continental iron flux and reverse weathering in the Proterozoic Eon: Insights from the Tonian Katherine Group, Yukon
Oolitic ironstones are iron-rich and chert-poor sedimentary rocks containing concentrically
coated grains composed of iron (oxyhydr) oxides and iron phyllosilicates that offer a unique …
coated grains composed of iron (oxyhydr) oxides and iron phyllosilicates that offer a unique …
Mud retention in hydrologically closed basins promoted pre-vegetation meandering: evidence from the Neoproterozoic Diabaig Formation, Scotland
Fluvial point-bar deposits are described from the c. 1 Ga Diabaig Formation, representing
some of the most compelling architectural evidence of planform sinuosity recognized in pre …
some of the most compelling architectural evidence of planform sinuosity recognized in pre …
Pre‐Vegetation Mixed (Wave‐Tide) Energy Trangressive Nearshore Sedimentation: Evidence From the Proterozoic Passive Margin Sequence of NW Himalaya, India
S Saha - Geological Journal, 2024 - Wiley Online Library
The coupled evolution of the Earth's atmosphere–biosphere system through time has
caused irreversible changes in the geodynamics as well as surface processes and …
caused irreversible changes in the geodynamics as well as surface processes and …
The early–middle Cambrian siliciclastic tide‐dominated succession in eastern Korea
Abstract The basal Taebaek Group (Myeonsan and Myobong formations) illustrates second‐
order transgression on the eastern Sino‐Korean Block during the early–middle Cambrian …
order transgression on the eastern Sino‐Korean Block during the early–middle Cambrian …
Palaeoenvironments of the Tonian to Cryogenian transition in the Adelaide Superbasin
G Virgo - 2023 - digital.library.adelaide.edu.au
The Neoproterozoic (~ 1000 to 539 Ma) was one of the most dynamic eras in Earth history
and was punctuated by significant tectonic, biological, atmospheric, and climatic events. This …
and was punctuated by significant tectonic, biological, atmospheric, and climatic events. This …