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- W2046603604 abstract "The object of this communication, is to present some observations on the succession and geological relations of the beds which have long been known in Trinidad as the Naparima Marls. This name was given to these beds by Wall & Sawkins in 1860, on account of their occupying a large part of the Naparima district, east and south-east of San Fernando (see map, fig. 1, p. 182). The beds so named formed one of the five series which were described by these authors under the head of the ‘Newer Parian Group.’ The names given to these five series were (<i>a</i>) Nariva Series, (<i>b</i>) Naparima Marls, (<i>c</i>) Tamana Series, (<i>d</i>) Caroni Series, and (<i>e</i>) Moruga Series; but it was explained on a subsequent page that these subdivisions do not form a definite succession. The Nariva Series occupies a central or axial position, and this Wall & Sawkins considered to be the oldest. The Tamana and the Caroni Series occur only to the north of it, while the Nariva and the Moruga lie on the southern side, and they thought that these two sets of deposits might be correlative one with another, the Nariva corresponding to the Tamana and the Moruga to the Caroni Series. In their general section across the island from north to south, Wall & Sawkins show the Nariva Beds dipping southward below the Naparima Marls, and the latter passing in the same direction beneath the Moraga sands ; while stiU farther south they indicate a syncline occupied by" @default.
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- W2046603604 date "1899-02-01" @default.
- W2046603604 modified "2023-10-16" @default.
- W2046603604 title "The Oceanic Deposits of Trinidad (British West Indies)" @default.
- W2046603604 doi "https://doi.org/10.1144/gsl.jgs.1899.055.01-04.12" @default.
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