| Reference Type | Journal (article/letter/editorial) |
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| Title | A low-temperature, meteoric water-dominated origin for smectitic clay minerals in the Chicxulub impact crater upper peak ring, as inferred from their oxygen and hydrogen isotope compositions |
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| Journal | Chemical Geology |
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| Authors | Simpson, S.L. | Author |
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| Longstaffe, F.J. | Author |
| Osinski, G.R. | Author |
| Caudill, C.M. | Author |
| Kring, D.A. | Author |
| Year | 2022 (January) | Volume | 588 |
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| Page(s) | 120639 |
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| Publisher | Elsevier BV |
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| DOI | doi:10.1016/j.chemgeo.2021.120639Search in ResearchGate |
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| Mindat Ref. ID | 15369226 | Long-form Identifier | mindat:1:5:15369226:2 |
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| GUID | 8ae803aa-02a0-46ba-ab2e-ebfba69af337 |
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| Full Reference | Simpson, S.L., Longstaffe, F.J., Osinski, G.R., Caudill, C.M., Kring, D.A. (2022) A low-temperature, meteoric water-dominated origin for smectitic clay minerals in the Chicxulub impact crater upper peak ring, as inferred from their oxygen and hydrogen isotope compositions. Chemical Geology, 588. 120639 doi:10.1016/j.chemgeo.2021.120639 |
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| Plain Text | Simpson, S.L., Longstaffe, F.J., Osinski, G.R., Caudill, C.M., Kring, D.A. (2022) A low-temperature, meteoric water-dominated origin for smectitic clay minerals in the Chicxulub impact crater upper peak ring, as inferred from their oxygen and hydrogen isotope compositions. Chemical Geology, 588. 120639 doi:10.1016/j.chemgeo.2021.120639 |
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| In | (2022) Chemical Geology Vol. 588. Elsevier BV |
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