Hammond, Douglas E., McManus, James, Berelson, William M., Meredith, Charlotte, Klinkhammer, Gary P., Coale, Kenneth H. (2000) Diagenetic fractionation of Ge and Si in reducing sediments: the missing Ge sink and a possible mechanism to cause glacial/interglacial variations in oceanic Ge/Si. Geochimica et Cosmochimica Acta, 64 (14) 2453-2465 doi:10.1016/s0016-7037(00)00362-8

| Reference Type | Journal (article/letter/editorial) | ||
|---|---|---|---|
| Title | Diagenetic fractionation of Ge and Si in reducing sediments: the missing Ge sink and a possible mechanism to cause glacial/interglacial variations in oceanic Ge/Si | ||
| Journal | Geochimica et Cosmochimica Acta | ||
| Authors | Hammond, Douglas E. | Author | |
| McManus, James | Author | ||
| Berelson, William M. | Author | ||
| Meredith, Charlotte | Author | ||
| Klinkhammer, Gary P. | Author | ||
| Coale, Kenneth H. | Author | ||
| Year | 2000 (July) | Volume | 64 |
| Issue | 14 | ||
| Publisher | Elsevier BV | ||
| DOI | doi:10.1016/s0016-7037(00)00362-8Search in ResearchGate | ||
| Generate Citation Formats | |||
| Mindat Ref. ID | 347754 | Long-form Identifier | mindat:1:5:347754:4 |
| GUID | 0 | ||
| Full Reference | Hammond, Douglas E., McManus, James, Berelson, William M., Meredith, Charlotte, Klinkhammer, Gary P., Coale, Kenneth H. (2000) Diagenetic fractionation of Ge and Si in reducing sediments: the missing Ge sink and a possible mechanism to cause glacial/interglacial variations in oceanic Ge/Si. Geochimica et Cosmochimica Acta, 64 (14) 2453-2465 doi:10.1016/s0016-7037(00)00362-8 | ||
| Plain Text | Hammond, Douglas E., McManus, James, Berelson, William M., Meredith, Charlotte, Klinkhammer, Gary P., Coale, Kenneth H. (2000) Diagenetic fractionation of Ge and Si in reducing sediments: the missing Ge sink and a possible mechanism to cause glacial/interglacial variations in oceanic Ge/Si. Geochimica et Cosmochimica Acta, 64 (14) 2453-2465 doi:10.1016/s0016-7037(00)00362-8 | ||
| In | (2000, July) Geochimica et Cosmochimica Acta Vol. 64 (14) Elsevier BV | ||
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