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- W1966498172 abstract "Abstract Zeolites and other amygdale minerals have a widespread occurrence in Martinique. The central and east part of the island is composed of pre-Pliocene submarine formations (hyaloclastitic tuffs, pillow lavas, swarms of dikes, and domes). Here, zeolites occur in about 10 well-defined areas where specific associations constitute discrete zones of progressive metamorphism. Four zones are established which are believed to reflect temperatures ranging from 100 to 200°C. Within the outer zone I, several of the following minerals occur together: heulandite or clinoptilolite, mordenite, chabazite, mesolite; analcime and thomsonite characterize a narrow zone II; stilbite is widespread in zone III, and laumontite characterizes inner zone IV. The Lamentin thermal area is mainly com posed of Recent monogenetic volcanoes (age The distribution of zeolites and other amygdale minerals is not related to regional metamorphism brought about by burial, but rather to areas of well-defined heat flow where suitable fluids were available. Roots of deeply eroded volcanoes, shallow magmatic intrusions, and zones of intensive faulting could have provided the necessary heat required; such structures are referred to in this communications as “heat flow domes”." @default.
- W1966498172 created "2016-06-24" @default.
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- W1966498172 date "1981-12-01" @default.
- W1966498172 modified "2023-10-02" @default.
- W1966498172 title "Distribution and volcano-structural control of zeolites and other amygdale minerals in the island of Martinique, F.W.I." @default.
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- W1966498172 doi "https://doi.org/10.1016/0377-0273(81)90031-7" @default.
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