1987
DOI: 10.1016/0899-5362(87)90036-4
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Apatite as a paleoenvironmental indicator in the Precambrian-mesozoic clastic sequence of the Middle East

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Cited by 8 publications
(1 citation statement)
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“…A‐apatites do not appear in strata younger than Devonian (Weissbrod & Nachmias, ), so Vermeesch et al. () and Weissbrod, Perath, and Nachmias () proposed that its growth resulted from a pulse of U‐rich hydrothermal fluid circulation related to the Palaeozoic thermal event. On the other hand, Segev () suggested a Neogene age for abundant U‐mineralisation and A‐apatite in Cambrian strata in southern Israel.…”
Section: Introductionmentioning
confidence: 99%
“…A‐apatites do not appear in strata younger than Devonian (Weissbrod & Nachmias, ), so Vermeesch et al. () and Weissbrod, Perath, and Nachmias () proposed that its growth resulted from a pulse of U‐rich hydrothermal fluid circulation related to the Palaeozoic thermal event. On the other hand, Segev () suggested a Neogene age for abundant U‐mineralisation and A‐apatite in Cambrian strata in southern Israel.…”
Section: Introductionmentioning
confidence: 99%