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Zhang, Chunxia, Guo, Zhengtang (2014) Clay mineral changes across the Eocene–Oligocene transition in the sedimentary sequence at Xining occurred prior to global cooling. Palaeogeography, Palaeoclimatology, Palaeoecology, 411. 18-29 doi:10.1016/j.palaeo.2014.06.031

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Reference TypeJournal (article/letter/editorial)
TitleClay mineral changes across the Eocene–Oligocene transition in the sedimentary sequence at Xining occurred prior to global cooling
JournalPalaeogeography, Palaeoclimatology, Palaeoecology
AuthorsZhang, ChunxiaAuthor
Guo, ZhengtangAuthor
Year2014 (October)Volume411
PublisherElsevier BV
DOIdoi:10.1016/j.palaeo.2014.06.031Search in ResearchGate
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Mindat Ref. ID938534Long-form Identifiermindat:1:5:938534:8
GUID0
Full ReferenceZhang, Chunxia, Guo, Zhengtang (2014) Clay mineral changes across the Eocene–Oligocene transition in the sedimentary sequence at Xining occurred prior to global cooling. Palaeogeography, Palaeoclimatology, Palaeoecology, 411. 18-29 doi:10.1016/j.palaeo.2014.06.031
Plain TextZhang, Chunxia, Guo, Zhengtang (2014) Clay mineral changes across the Eocene–Oligocene transition in the sedimentary sequence at Xining occurred prior to global cooling. Palaeogeography, Palaeoclimatology, Palaeoecology, 411. 18-29 doi:10.1016/j.palaeo.2014.06.031
In(2014) Palaeogeography, Palaeoclimatology, Palaeoecology Vol. 411. Elsevier BV

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