Diagenetic and hydrothermal events revealed by an Ediacaran dolomite breccia from the Araras-Alto Paraguai Basin, Southern Amazon Craton

Author:

Sepeda L.F.ORCID,Nogueira A.C.R.,Santos R.F. dos,Okubo J.,Silva P.A.S.,Marques J.C.,Milhomem J.M.N.,Luvizotto G.L.,Macambira M.J.B.,Sial A.N.

Funder

CNPq

Publisher

Elsevier BV

Reference88 articles.

1. An early diagenetic deglacial origin for basal Ediacaran “cap dolostones”;Ahm;Earth Planet Sci. Lett.,2019

2. Origin and characterization of hydrothermal dolomite in the Western Canada Sedimentary Basin;Al-Aasm;Journal of Geochemical Exploration 78-79,2003

3. Dolomite Reservoirs: Geochemical Techniques for Evaluating Origin and Distribution;Allan;American Association of Petroleum Geologists, Continuing Education Course Notes,1993

4. Origem e Evolução da Plataforma brasileira. Rio de Janeiro, DNPM;Almeida;Boletim da Divisão de Geologia e Mineralogia,1967

5. Alvarenga C.J.S., Trompette R. 1988. Upper Proterozoic glacial environment of the border of Amazonian Craton and its evolution towards the adjacent Paraguay Belt (Mato Grosso, Brazil). In: Meeting of earth glacial record. Abstract and field trip. IGCP-UNESCO/UFMT, 260, p. 31-44.

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