Re-Os and Lu-Hf isotope constraints on the origin and age of pyroxenites from the Beni Bousera peridotite massif: implications for mixed peridotite-pyroxenite melting models

Pearson, D.G; Nowell, G.M

doi:10.1093/petrology/egg102

All Outputs (3)

Phase I and Pharmacodynamic Study of Fludarabine, Carboplatin, and Topotecan in Patients with Relapsed, Refractory or High Risk Acute Leukemia and Advanced Myelodysplastic Syndromes. (2004)
Journal Article
Cooper, B., Veal, G., Radivoyevitch, T., Tilby, M., Meyerson, H., Lazarus, H., …Gerson, S. (2004). Phase I and Pharmacodynamic Study of Fludarabine, Carboplatin, and Topotecan in Patients with Relapsed, Refractory or High Risk Acute Leukemia and Advanced Myelodysplastic Syndromes. Clinical Cancer Research, 10, 6830-6839

Hf isotope systematics of kimberlites and their megacrysts: New constraints on their source regions (2004)
Journal Article
Nowell, G., Pearson, D., Bell, D., Carlson, R., Smith, C., Kempton, P., & Noble, S. (2004). Hf isotope systematics of kimberlites and their megacrysts: New constraints on their source regions. Journal of Petrology, 45(8), 1583-1612. https://doi.org/10.1093/petrology/egh024

Kimberlites from Southern Africa, along with their low-Cr megacrysts, have unusual Hf–Nd isotopic characteristics. Group I and Transitional kimberlites define arrays trending oblique to, and well below, the Nd–Hf isotope ‘mantle array’, defined by oc... Read More about Hf isotope systematics of kimberlites and their megacrysts: New constraints on their source regions.

Re-Os and Lu-Hf isotope constraints on the origin and age of pyroxenites from the Beni Bousera peridotite massif: implications for mixed peridotite-pyroxenite melting models (2004)
Journal Article
Pearson, D., & Nowell, G. (2004). Re-Os and Lu-Hf isotope constraints on the origin and age of pyroxenites from the Beni Bousera peridotite massif: implications for mixed peridotite-pyroxenite melting models. Journal of Petrology, 45(2), 439-455. https://doi.org/10.1093/petrology/egg102

A suite of pyroxenites from the Beni Bousera peridotite massif, northern Morocco, have been analysed for Re–Os and Lu–Hf isotopic compositions. Measured sections of the massif indicate that pyroxenite layers make up between 1 and 9% by volume of the... Read More about Re-Os and Lu-Hf isotope constraints on the origin and age of pyroxenites from the Beni Bousera peridotite massif: implications for mixed peridotite-pyroxenite melting models.