Comparisons of the Paleo-Mesoproterozoic large igneous provinces and black shales in the North China and North Australian cratons [PDF]
Comparisons of large igneous provinces (LIPs) and black shales from different cratons can provide important constraints on Precambrian paleogeographic reconstructions and a better understanding of the environmental effects of large-scale volcanic events.
Shuan-Hong Zhang+8 more
doaj +2 more sources
Organic vs inorganic contribution to the chemistry of cretaceous black shales in the Mamfe basin, SW Cameroon. Evidence from geochemistry and statistical analysis [PDF]
The present study focused on evaluating the contribution of both organic and inorganic component to the chemistry of Cretaceous black shales in the Mamfe basin, Sw Cameroon by performing inductively couple plasma spectrometry analyses with the data ...
Bisse Salomon Betrant+9 more
doaj +2 more sources
Cu isotopes in marine black shales record the Great Oxidation Event. [PDF]
Significance Redox-sensitive transition metals and their isotopes provide some of the best lines of evidence for reconstructing early Earth’s oxygenation history, including permanent atmospheric oxygenation following the Great Oxidation Event (GOE), ∼2 ...
Chi Fru E+8 more
europepmc +2 more sources
Experimental Investigation of Mechanical Properties of Black Shales after CO₂-Water-Rock Interaction. [PDF]
The effects of CO2-water-rock interactions on the mechanical properties of shale are essential for estimating the possibility of sequestrating CO2 in shale reservoirs.
Lyu Q, Ranjith PG, Long X, Ji B.
europepmc +2 more sources
Phanerozoic environments of black shale deposition and the Wilson Cycle [PDF]
The spatial and temporal distribution of black shales is related to the development of environments in which they accumulate and to a propitious combination of environmental variables.
J. Trabucho-Alexandre+2 more
doaj +5 more sources
Tellurium, selenium and cobalt enrichment in Neoproterozoic black shales, Gwna Group, UK : Deep marine trace element enrichment during the Second Great Oxygenation Event [PDF]
We are grateful to John Still for his skilled technical support and the ACEMAC facility at the University of Aberdeen. Research funded by NERC grant NE/M010953/1 and NERC facility grant IP-1631-0516. AJB is funded by NERC support of the Isotope Community
Armstrong, Joseph+5 more
core +3 more sources
Paleoclimate characteristics of source area weathering and metallogenic implication of cretaceous black shales in the Mamfe basin, (SW Cameroon): Evidence from lithogeochemistry [PDF]
Black shales are highly enriched in essential elements containing critical information on metallic richness and paleoclimatic imprints during deposition.
Bokanda Ekoko Eric+5 more
doaj +2 more sources
Environmental impact of mineralised black shales
Black shales are sedimentary rocks containing >0.5% of organic carbon. They host polymetallic deposits which have been mined for Cu, Ni, Zn, Mn, P, Mo, V, U, Au and PGE (platinum group elements). Even sub-economic occurrences provide potential risk of acid rock drainage when exposed to oxic surface environment. The natural acid neutralisation potential
Kirsti Loukola-Ruskeeniemi+2 more
openaire +5 more sources
The origin of Cretaceous black shales: a change in the surface ocean ecosystem and its triggers. [PDF]
Black shale is dark-colored, organic-rich sediment, and there have been many episodes of black shale deposition over the history of the Earth. Black shales are source rocks for petroleum and natural gas, and thus are both geologically and economically ...
Ohkouchi N, Kuroda J, Taira A.
europepmc +2 more sources
Lower Wenlock black shales in the northern Holy Cross Mountains, Poland: Sedimentary and geochemical controls on the Ireviken Event in a deep marine setting [PDF]
The stratigraphic variability and geochemistry of Llandovery/Wenlock (L/W) Series boundary sediments in Poland reveals that hemipelagic sedimentation under an anoxic/euxinic water column was interrupted by low density bottom currents or detached diluted ...
Bond, David P. G.+3 more
core +2 more sources