Economic Geology of the Tumpa Gold Deposit (New California)
DOI:
https://doi.org/10.15381/iigeo.v2i4.2154Keywords:
Tumpa, granodiorite, batholith of the Cordillera Blanca, gold depositAbstract
The Tumpa gold deposit, operated by Cia. Minera Nueva California, located on the western flank of the Cordillera Blanca; It is a vein located between the intensely argilized granodiorite of the Cordillera Blanca batholith and a silicified andesitic dam. The mineralizing flow in its upper part was horizontal with a higher concentration of gold. The vein and dike were cut into 3 parts according to their direction by 2 similar faults to the vein and dike, of dip contrary to these structures; they have intense oxidation.
Downloads
Published
Issue
Section
License
Copyright (c) 1999 Pedro Hugo Tumialán de la Cruz
![Creative Commons License](http://i.creativecommons.org/l/by-nc-sa/4.0/88x31.png)
This work is licensed under a Creative Commons Attribution-NonCommercial-ShareAlike 4.0 International License.
AUTHORS RETAIN THEIR RIGHTS:
a. Authors retain their trade mark rights and patent, and also on any process or procedure described in the article.
b. Authors retain their right to share, copy, distribute, perform and publicly communicate their article (eg, to place their article in an institutional repository or publish it in a book), with an acknowledgment of its initial publication in the Rev. Inst. investig. Fac. minas metal cienc. geogr.
c. Authors retain theirs right to make a subsequent publication of their work, to use the article or any part thereof (eg a compilation of his papers, lecture notes, thesis, or a book), always indicating the source of publication (the originator of the work, journal, volume, number and date).