Sedimentologic development of a Late Oligocene–Miocene forearc embayment, Valdivia Basin Complex, southern Chile

Author:

le Roux J.P,Elgueta Sara

Publisher

Elsevier BV

Subject

Stratigraphy,Geology

Reference58 articles.

1. Alfaro, G., Cisternas, M.E., 1995. Chemical and mineralogical characteristics of the sub-bituminous coal of the Oligo–Miocene of southern-center Chile (X Region). In: Pajares, J.A., Tascon, J.M.D. (Eds.), Coal Science: Proceedings of the Eighth International Conference on Coal Science. Elsevier, Amsterdam, pp. 103–106.

2. Alfaro, G., Gantz, E., Magna, O., 1990. El yacimiento de carbón Catamutún (La Union). 2° Simposio sobre el Terciario de Chile, Concepción, Actas, Vol. 1, pp. 11–28.

3. Baldis, A.J., Febrer, J., 1983. Geodynamics of the Andean Arc and related regions. In: Cabré, R. (Ed.), Geodynamics of the Eastern Pacific Region, Caribbean and Scotia Arcs. Am. Geophys. Union, Geodyn. Ser. 9, 127–135.

4. Blow, W., 1969. Late Middle Eocene to Recent planktonic foraminiferal biostratigraphy. In: Proceedings of the First International Conference on Planktonic Microfossils. Brill, Leiden, Vol. 1, pp. 199–422.

5. Boron in illite as a paleosalinity indicator of Illinois coal;Bohor;J. Sediment. Petrol.,1973

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