2003
DOI: 10.1016/j.jafrearsci.2003.08.002
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Distribution patterns of rare-earth elements and uranium in tertiary sedimentary phosphorites of Hahotoé–Kpogamé, Togo

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Cited by 42 publications
(22 citation statements)
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“…The diffractogram, presented in Fig. 2 [17], [18]. It appears that the recorded dolomite, calcite and quartz phases due to their nature exogangue, while the interference of these phases with fluorapatite are due to their natural endogangue.…”
Section: Xrd Analysis and Phases Identificationmentioning
confidence: 92%
“…The diffractogram, presented in Fig. 2 [17], [18]. It appears that the recorded dolomite, calcite and quartz phases due to their nature exogangue, while the interference of these phases with fluorapatite are due to their natural endogangue.…”
Section: Xrd Analysis and Phases Identificationmentioning
confidence: 92%
“…It is known that mineral weathering is an important source of elements to the soils [43]. However, even after weathering of primary minerals, REE can still, partially or totally, be again incorporated in secondary minerals, remaining immobilized [44].…”
Section: Sources and Fate Of Ree In Soilsmentioning
confidence: 99%
“…Once released from primary minerals, REEs are either lost from the weathering profile via the soil solution or incorporated, partially or totally, into secondary minerals that may be subsequently weathered (Öhlander et al, 1996;Panahi et al, 2000;Taunton et al, 2000;Gnandi and Tobschall, 2003). The REE redistribution during weathering is a function of:…”
Section: Impact Of Weathering On Ree Mobilizationmentioning
confidence: 99%