Contribution to the understanding of the structure of Aljustrel mine Iberian Pyrite Belt, based in new palynostratigraphical data obtained in the Volcano-Sedimentary Complex and Mértola Formation.

João Xavier Matos; Zélia Pereira; Paulo Fernandes; Diogo Raeymaekers Namorado Rosa; Jose Tomas Oliveira

Contribution to the understanding of the structure of Aljustrel mine Iberian Pyrite Belt, based in new palynostratigraphical data obtained in the Volcano-Sedimentary Complex and Mértola Formation.

João Xavier Matos
, Zélia Pereira
, Paulo Fernandes
, Diogo Raeymaekers Namorado Rosa
, Jose Tomas Oliveira

Research output: Chapter in Book/Report/Conference proceeding › Conference article in proceedings › peer-review

Abstract

Palynostratigraphic analysis and detailed mapping of the Volcano-Sedimentary Complex
sedimentary formations and the Mértola Formation (Baixo Alentejo Flysch), in the Aljustrel mining area of the Iberian Pyrite Belt, permit a better understanding of the local structure. The Paraíso Formation shows an upper Tournaisian to upper Viséan age (CM and Pu Miospores Biozones). The Gavião Formation presents a similar age (upper Tournaisian, CM Biozone). A new unit is proposed representing the base of the Mértola Formation, the Canal da BAI Unit (upper middle Viséan age, NM biozone).

Original language	English
Title of host publication	e-Terra
Subtitle of host publication	Geosciences On-line Journal
Number of pages	4
Volume	21
Edition	10
Publication status	Published - 2010
Externally published	Yes
Event	VIII Congresso Nacional de Geologia: Portugal - Braga, Portugal Duration: 9 Jul 2010 → 16 Jul 2010 http://www.dct.uminho.pt/cng2010/inicio/inicio.html

Conference

Conference	VIII Congresso Nacional de Geologia
Country/Territory	Portugal
City	Braga
Period	9/07/10 → 16/07/10
Internet address	http://www.dct.uminho.pt/cng2010/inicio/inicio.html

UN SDGs

This output contributes to the following UN Sustainable Development Goals (SDGs)

SDG 7 Affordable and Clean Energy

Programme Area

Programme Area 4: Mineral Resources

Access to Document

https://repositorio.lneg.pt/bitstream/10400.9/1257/1/34367.pdf

Cite this

Matos, J. X., Pereira, Z., Fernandes, P., Rosa, D. R. N., & Oliveira, J. T. (2010). Contribution to the understanding of the structure of Aljustrel mine Iberian Pyrite Belt, based in new palynostratigraphical data obtained in the Volcano-Sedimentary Complex and Mértola Formation. In e-Terra: Geosciences On-line Journal (10 ed., Vol. 21) https://repositorio.lneg.pt/bitstream/10400.9/1257/1/34367.pdf

@inproceedings{6b11201d4399451d97c3696bfead0a59,

title = "Contribution to the understanding of the structure of Aljustrel mine Iberian Pyrite Belt, based in new palynostratigraphical data obtained in the Volcano-Sedimentary Complex and M{\'e}rtola Formation.",

abstract = "Palynostratigraphic analysis and detailed mapping of the Volcano-Sedimentary Complex sedimentary formations and the M{\'e}rtola Formation (Baixo Alentejo Flysch), in the Aljustrel mining area of the Iberian Pyrite Belt, permit a better understanding of the local structure. The Para{\'i}so Formation shows an upper Tournaisian to upper Vis{\'e}an age (CM and Pu Miospores Biozones). The Gavi{\~a}o Formation presents a similar age (upper Tournaisian, CM Biozone). A new unit is proposed representing the base of the M{\'e}rtola Formation, the Canal da BAI Unit (upper middle Vis{\'e}an age, NM biozone).",

author = "Matos, \{Jo{\~a}o Xavier\} and Z{\'e}lia Pereira and Paulo Fernandes and Rosa, \{Diogo Raeymaekers Namorado\} and Oliveira, \{Jose Tomas\}",

year = "2010",

language = "English",

volume = "21",

booktitle = "e-Terra",

edition = "10",

note = "VIII Congresso Nacional de Geologia : Portugal ; Conference date: 09-07-2010 Through 16-07-2010",

url = "http://www.dct.uminho.pt/cng2010/inicio/inicio.html",

}

Matos, JX, Pereira, Z, Fernandes, P, Rosa, DRN & Oliveira, JT 2010, Contribution to the understanding of the structure of Aljustrel mine Iberian Pyrite Belt, based in new palynostratigraphical data obtained in the Volcano-Sedimentary Complex and Mértola Formation. in e-Terra: Geosciences On-line Journal. 10 edn, vol. 21, VIII Congresso Nacional de Geologia, Braga, Portugal, 9/07/10. <https://repositorio.lneg.pt/bitstream/10400.9/1257/1/34367.pdf>

Contribution to the understanding of the structure of Aljustrel mine Iberian Pyrite Belt, based in new palynostratigraphical data obtained in the Volcano-Sedimentary Complex and Mértola Formation. / Matos, João Xavier; Pereira, Zélia; Fernandes, Paulo et al.
e-Terra: Geosciences On-line Journal. Vol. 21 10. ed. 2010.

Research output: Chapter in Book/Report/Conference proceeding › Conference article in proceedings › peer-review

TY - GEN

T1 - Contribution to the understanding of the structure of Aljustrel mine Iberian Pyrite Belt, based in new palynostratigraphical data obtained in the Volcano-Sedimentary Complex and Mértola Formation.

AU - Matos, João Xavier

AU - Pereira, Zélia

AU - Fernandes, Paulo

AU - Rosa, Diogo Raeymaekers Namorado

AU - Oliveira, Jose Tomas

PY - 2010

Y1 - 2010

N2 - Palynostratigraphic analysis and detailed mapping of the Volcano-Sedimentary Complex sedimentary formations and the Mértola Formation (Baixo Alentejo Flysch), in the Aljustrel mining area of the Iberian Pyrite Belt, permit a better understanding of the local structure. The Paraíso Formation shows an upper Tournaisian to upper Viséan age (CM and Pu Miospores Biozones). The Gavião Formation presents a similar age (upper Tournaisian, CM Biozone). A new unit is proposed representing the base of the Mértola Formation, the Canal da BAI Unit (upper middle Viséan age, NM biozone).

AB - Palynostratigraphic analysis and detailed mapping of the Volcano-Sedimentary Complex sedimentary formations and the Mértola Formation (Baixo Alentejo Flysch), in the Aljustrel mining area of the Iberian Pyrite Belt, permit a better understanding of the local structure. The Paraíso Formation shows an upper Tournaisian to upper Viséan age (CM and Pu Miospores Biozones). The Gavião Formation presents a similar age (upper Tournaisian, CM Biozone). A new unit is proposed representing the base of the Mértola Formation, the Canal da BAI Unit (upper middle Viséan age, NM biozone).

M3 - Conference article in proceedings

VL - 21

BT - e-Terra

T2 - VIII Congresso Nacional de Geologia

Y2 - 9 July 2010 through 16 July 2010

ER -

Contribution to the understanding of the structure of Aljustrel mine Iberian Pyrite Belt, based in new palynostratigraphical data obtained in the Volcano-Sedimentary Complex and Mértola Formation.

Abstract

Conference

UN SDGs

Programme Area

Access to Document

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Cite this