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Vinogradov, V. I. (2008) Carbon and oxygen isotopic composition of the Vendian-Cambrian carbonate rocks and paleoecological reconstructions. Lithology and Mineral Resources, 43 (1) 44-57 doi:10.1134/s0024490208010045

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Reference TypeJournal (article/letter/editorial)
TitleCarbon and oxygen isotopic composition of the Vendian-Cambrian carbonate rocks and paleoecological reconstructions
JournalLithology and Mineral Resources
AuthorsVinogradov, V. I.Author
Year2008 (January)Volume43
Issue1
PublisherPleiades Publishing Ltd
DOIdoi:10.1134/s0024490208010045Search in ResearchGate
Generate Citation Formats
Mindat Ref. ID158376Long-form Identifiermindat:1:5:158376:6
GUID0
Full ReferenceVinogradov, V. I. (2008) Carbon and oxygen isotopic composition of the Vendian-Cambrian carbonate rocks and paleoecological reconstructions. Lithology and Mineral Resources, 43 (1) 44-57 doi:10.1134/s0024490208010045
Plain TextVinogradov, V. I. (2008) Carbon and oxygen isotopic composition of the Vendian-Cambrian carbonate rocks and paleoecological reconstructions. Lithology and Mineral Resources, 43 (1) 44-57 doi:10.1134/s0024490208010045
In(2008, January) Lithology and Mineral Resources Vol. 43 (1) Pleiades Publishing Ltd

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Vinogradov, V. I., Belenitskaya, G. A., Bujakaite, M. I., Kuleshov, V. N., Minaeva, M. A., Pokrovskii, B. G. (2006) Isotopic signatures of deposition and transformation of Lower Cambrian saliferous rocks in the Irkutsk amphitheater: Communication 1. Sulfur isotopic composition. Lithology and Mineral Resources, 41 (1) 85-97 doi:10.1134/s002449020601007x
Vinogradov, V. I. (2009) Possibilities and limitations of isotopic chemostratigraphy. Lithology and Mineral Resources, 44 (3) 245-257 doi:10.1134/s0024490209030031
Vinogradov, V. I., Belenitskaya, G. A., Bujakaite, M. I., Kuleshov, V. N., Minaeva, M. A., Pokrovskii, B. G. (2006) Isotopic signatures of deposition and transformation of Lower Cambrian saliferous rocks in the Irkutsk Amphitheater: Communication 3. Carbon and oxygen isotopic compositions in carbonates. Lithology and Mineral Resources, 41 (3) 271-279 doi:10.1134/s0024490206030060
Vinogradov, V. I., Belenitskaya, G. A., Bujakaite, M. I., Kuleshov, V. N., Minaeva, M. A., Pokrovskii, B. G. (2006) Isotopic signatures of deposition and transformation of Lower Cambrian saliferous rocks in the Irkutsk amphitheater: Communication 2. Strontium isotopic composition. Lithology and Mineral Resources, 41 (2) 165-173 doi:10.1134/s0024490206020052
Vinogradov, V. I. (2007) Was there a conflict at the Neoproterozoic-Cambrian boundary: Evidence from sulfur isotope composition?. Lithology and Mineral Resources, 42 (1) 1-14 doi:10.1134/s0024490207010014
Vinogradov, V. I., Golovin, D. I. (2008) Geochemical significance of K-Ar geochronological investigations of sedimentary rocks. Lithology and Mineral Resources, 43 (2) 154-164 doi:10.1134/s0024490208020053
Vinogradov, V. I., Belenitskaya, G. A., Pokrovsky, B. G., Bujakaite, M. I. (2011) Isotopic-geochemical features of rocks of the Middle-Upper Cambrian Verkhnyaya Lena formation in the Siberian Craton. Lithology and Mineral Resources, 46 (1) 71-84 doi:10.1134/s0024490210061021
Felitsyn, S. B. (2008) Gold in Vendian-Cambrian organic macrofossils of the East European platform. Lithology and Mineral Resources, 43 (6) 542-548 doi:10.1134/s0024490208060035
Vinogradov, V. I., Belenitskaya, G. A., Bujakaite, M. I., Golovin, D. I., Kuleshov, V. N., Minaeva, M. A. (2006) Isotopic evidence for postsedimentary transformation of rocks of the Lower Cambrian Angara Formation in the Irkutsk Amphitheater. Lithology and Mineral Resources, 41 (6) 588-600 doi:10.1134/s0024490206060071
Maslov, A. V., Podkovyrov, V. N. (2023) Chemical Weathering Indexes: Implication for Paleoclimatic Reconstructions, with the Vendian–Lower Cambrian Section of Podolian Transnistria as Example. Lithology and Mineral Resources, 58 (3) 213-234 doi:10.1134/s0024490222700043
Felitsyn, S. B. (2006) Alkali earth elements in Vendian-Cambrian clayey rocks, the East European Platform. Lithology and Mineral Resources, 41 (4) 362-370 doi:10.1134/s0024490206040067
 
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