Chromite deposits at Loma Baya: petrogenesis and clues for the origin of the coastal Guerrero Composite Terrane in Mexico

Jose Gonzalez-Jimenez; Joaquín A. Proenza; Antoni Camprubí; Elena Centeno-García; Eduardo González-Partida; Bill Griffin; Sue O'Reilly; Norman Pearson

Chromite deposits at Loma Baya: petrogenesis and clues for the origin of the coastal Guerrero Composite Terrane in Mexico

Jose Gonzalez-Jimenez, Joaquín A. Proenza, Antoni Camprubí, Elena Centeno-García, Eduardo González-Partida, Bill Griffin, Sue O'Reilly, Norman Pearson

ARC Centre of Excellence for Core to Crust Fluid Systems (incorporation ARC National Key Centre for Geochemical evolution and Metallogeny of Continents (GEMOC))

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

Abstract

The high-Al podiform Loma Baya chromitite deposits occur hosted within an ultramafic massif representative of ophiolitic mantle produced in a back-arc basin near to the westernmost edge of the Guerrero Composite Terrane, SW Mexico. Such conclusion is drawn from the tholeiitic (i.e., back-arc basin basalt) affinity of the parental melts of the chromitite, deduced from major and trace element distribution in chromite, and the nature of the platinum-group elements mineralization.

Original language	English
Title of host publication	Let's talk ore deposits
Subtitle of host publication	proceedings of the Eleventh Biennial SGA Meeting
Editors	Fernando Barra, Martin Reich, Eduardo Campos, Fernando Tornos
Place of Publication	Antofagasta, Chile
Publisher	Ediciones Universidad Católica del Nort
Pages	604-606
Number of pages	3
ISBN (Print)	9789562873291
Publication status	Published - 2011
Event	11th SGA Biennial Meeting - Antofagasta, Chile Duration: 26 Sep 2011 → 29 Sep 2011

Conference

Conference	11th SGA Biennial Meeting
Country/Territory	Chile
City	Antofagasta
Period	26/09/11 → 29/09/11

Keywords

chromite deposit
platinum-group elements
ophiolite
back-arc basin
Loma Baya
Guerrero Composite Terrane
Mexico

Cite this

Gonzalez-Jimenez, J., Proenza, J. A., Camprubí, A., Centeno-García, E., González-Partida, E., Griffin, B., O'Reilly, S., & Pearson, N. (2011). Chromite deposits at Loma Baya: petrogenesis and clues for the origin of the coastal Guerrero Composite Terrane in Mexico. In F. Barra, M. Reich, E. Campos, & F. Tornos (Eds.), Let's talk ore deposits: proceedings of the Eleventh Biennial SGA Meeting (pp. 604-606). Ediciones Universidad Católica del Nort.

Gonzalez-Jimenez, Jose ; Proenza, Joaquín A. ; Camprubí, Antoni ; Centeno-García, Elena ; González-Partida, Eduardo ; Griffin, Bill ; O'Reilly, Sue ; Pearson, Norman. / Chromite deposits at Loma Baya : petrogenesis and clues for the origin of the coastal Guerrero Composite Terrane in Mexico. Let's talk ore deposits: proceedings of the Eleventh Biennial SGA Meeting. editor / Fernando Barra ; Martin Reich ; Eduardo Campos ; Fernando Tornos. Antofagasta, Chile : Ediciones Universidad Católica del Nort, 2011. pp. 604-606

@inproceedings{2d5cd0f2102f48cd9479b3ebf42de96b,

title = "Chromite deposits at Loma Baya: petrogenesis and clues for the origin of the coastal Guerrero Composite Terrane in Mexico",

abstract = "The high-Al podiform Loma Baya chromitite deposits occur hosted within an ultramafic massif representative of ophiolitic mantle produced in a back-arc basin near to the westernmost edge of the Guerrero Composite Terrane, SW Mexico. Such conclusion is drawn from the tholeiitic (i.e., back-arc basin basalt) affinity of the parental melts of the chromitite, deduced from major and trace element distribution in chromite, and the nature of the platinum-group elements mineralization.",

keywords = "chromite deposit, platinum-group elements, ophiolite, back-arc basin, Loma Baya, Guerrero Composite Terrane, Mexico",

author = "Jose Gonzalez-Jimenez and Proenza, {Joaqu{\'i}n A.} and Antoni Camprub{\'i} and Elena Centeno-Garc{\'i}a and Eduardo Gonz{\'a}lez-Partida and Bill Griffin and Sue O'Reilly and Norman Pearson",

year = "2011",

language = "English",

isbn = "9789562873291",

pages = "604--606",

editor = "Fernando Barra and Martin Reich and Eduardo Campos and Fernando Tornos",

booktitle = "Let's talk ore deposits",

publisher = "Ediciones Universidad Cat{\'o}lica del Nort",

note = "11th SGA Biennial Meeting ; Conference date: 26-09-2011 Through 29-09-2011",

}

Gonzalez-Jimenez, J, Proenza, JA, Camprubí, A, Centeno-García, E, González-Partida, E, Griffin, B , O'Reilly, S & Pearson, N 2011, Chromite deposits at Loma Baya: petrogenesis and clues for the origin of the coastal Guerrero Composite Terrane in Mexico. in F Barra, M Reich, E Campos & F Tornos (eds), Let's talk ore deposits: proceedings of the Eleventh Biennial SGA Meeting. Ediciones Universidad Católica del Nort, Antofagasta, Chile, pp. 604-606, 11th SGA Biennial Meeting, Antofagasta, Chile, 26/09/11.

Chromite deposits at Loma Baya : petrogenesis and clues for the origin of the coastal Guerrero Composite Terrane in Mexico. / Gonzalez-Jimenez, Jose; Proenza, Joaquín A.; Camprubí, Antoni; Centeno-García, Elena; González-Partida, Eduardo; Griffin, Bill ; O'Reilly, Sue; Pearson, Norman.

Let's talk ore deposits: proceedings of the Eleventh Biennial SGA Meeting. ed. / Fernando Barra; Martin Reich; Eduardo Campos; Fernando Tornos. Antofagasta, Chile : Ediciones Universidad Católica del Nort, 2011. p. 604-606.

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

TY - GEN

T1 - Chromite deposits at Loma Baya

T2 - 11th SGA Biennial Meeting

AU - Gonzalez-Jimenez, Jose

AU - Proenza, Joaquín A.

AU - Camprubí, Antoni

AU - Centeno-García, Elena

AU - González-Partida, Eduardo

AU - Griffin, Bill

AU - O'Reilly, Sue

AU - Pearson, Norman

PY - 2011

Y1 - 2011

N2 - The high-Al podiform Loma Baya chromitite deposits occur hosted within an ultramafic massif representative of ophiolitic mantle produced in a back-arc basin near to the westernmost edge of the Guerrero Composite Terrane, SW Mexico. Such conclusion is drawn from the tholeiitic (i.e., back-arc basin basalt) affinity of the parental melts of the chromitite, deduced from major and trace element distribution in chromite, and the nature of the platinum-group elements mineralization.

AB - The high-Al podiform Loma Baya chromitite deposits occur hosted within an ultramafic massif representative of ophiolitic mantle produced in a back-arc basin near to the westernmost edge of the Guerrero Composite Terrane, SW Mexico. Such conclusion is drawn from the tholeiitic (i.e., back-arc basin basalt) affinity of the parental melts of the chromitite, deduced from major and trace element distribution in chromite, and the nature of the platinum-group elements mineralization.

KW - chromite deposit

KW - platinum-group elements

KW - ophiolite

KW - back-arc basin

KW - Loma Baya

KW - Guerrero Composite Terrane

KW - Mexico

M3 - Conference proceeding contribution

SN - 9789562873291

SP - 604

EP - 606

BT - Let's talk ore deposits

A2 - Barra, Fernando

A2 - Reich, Martin

A2 - Campos, Eduardo

A2 - Tornos, Fernando

PB - Ediciones Universidad Católica del Nort

CY - Antofagasta, Chile

Y2 - 26 September 2011 through 29 September 2011

ER -

Gonzalez-Jimenez J, Proenza JA, Camprubí A, Centeno-García E, González-Partida E, Griffin B et al. Chromite deposits at Loma Baya: petrogenesis and clues for the origin of the coastal Guerrero Composite Terrane in Mexico. In Barra F, Reich M, Campos E, Tornos F, editors, Let's talk ore deposits: proceedings of the Eleventh Biennial SGA Meeting. Antofagasta, Chile: Ediciones Universidad Católica del Nort. 2011. p. 604-606

Chromite deposits at Loma Baya: petrogenesis and clues for the origin of the coastal Guerrero Composite Terrane in Mexico

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