Raman study of several Cu-bearing complex minerals from the guano deposit at Pabellón de Pica, Tarapaca region, Chile

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216208%3A11310%2F23%3A10477735" target="_blank" >RIV/00216208:11310/23:10477735 - isvavai.cz</a>

Výsledek na webu

<a href="https://verso.is.cuni.cz/pub/verso.fpl?fname=obd_publikace_handle&handle=c~Sl.oNCBY" target="_blank" >https://verso.is.cuni.cz/pub/verso.fpl?fname=obd_publikace_handle&handle=c~Sl.oNCBY</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.1002/jrs.6506" target="_blank" >10.1002/jrs.6506</a>

Jazyk výsledku

angličtina

Název v původním jazyce

Raman study of several Cu-bearing complex minerals from the guano deposit at Pabellón de Pica, Tarapaca region, Chile

Popis výsledku v původním jazyce

Pabellón de Pica, Tarapaca, Chile, is a former guano mine exploited in the late 19th and early 20th centuries. Guano is in a direct contact with Cu sulfide mineralization leading to the formation of minerals with a highly unusual chemical composition, especially Cu-organic complexes and nitrogen-bearing phases. In this work, we report results of the Raman spectroscopic investigation of several unique Cu-bearing minerals that are the result of supergene processes at the Pabellon da Pica site. We focus on several minerals with new and interesting structure types which were described from this locality for the first time, namely, antipinite (K-Na-Cu oxalate), ammineite (Cu ammine complex), chanabayaite (Cu ammine triazolate complex), and joanneumite (Cu isocyanurate). The Raman spectra contain specific bands attributed to the characteristic vibrations of the molecular groups present in the minerals (oxalate, ammine, triazolate, and isocyanurate groups) and vibrations within Cu-centered polyhedra. A comparison was made with the vibrational spectra of related minerals and synthetic phases, which revealed substantial proliferation and shifting of numerous bands, which is in agreement with the complex composition of the investigated minerals. The results obtained appropriately complement known structural and spectroscopic data published previously.

Název v anglickém jazyce

Raman study of several Cu-bearing complex minerals from the guano deposit at Pabellón de Pica, Tarapaca region, Chile

Popis výsledku anglicky

Pabellón de Pica, Tarapaca, Chile, is a former guano mine exploited in the late 19th and early 20th centuries. Guano is in a direct contact with Cu sulfide mineralization leading to the formation of minerals with a highly unusual chemical composition, especially Cu-organic complexes and nitrogen-bearing phases. In this work, we report results of the Raman spectroscopic investigation of several unique Cu-bearing minerals that are the result of supergene processes at the Pabellon da Pica site. We focus on several minerals with new and interesting structure types which were described from this locality for the first time, namely, antipinite (K-Na-Cu oxalate), ammineite (Cu ammine complex), chanabayaite (Cu ammine triazolate complex), and joanneumite (Cu isocyanurate). The Raman spectra contain specific bands attributed to the characteristic vibrations of the molecular groups present in the minerals (oxalate, ammine, triazolate, and isocyanurate groups) and vibrations within Cu-centered polyhedra. A comparison was made with the vibrational spectra of related minerals and synthetic phases, which revealed substantial proliferation and shifting of numerous bands, which is in agreement with the complex composition of the investigated minerals. The results obtained appropriately complement known structural and spectroscopic data published previously.

Druh

J_imp - Článek v periodiku v databázi Web of Science

CEP obor

—

OECD FORD obor

10505 - Geology

Projekt

—

Návaznosti

I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Rok uplatnění

2023

Kód důvěrnosti údajů

S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Název periodika

Journal of Raman Spectroscopy

ISSN

0377-0486

e-ISSN

1097-4555

Svazek periodika

54

Číslo periodika v rámci svazku

11

Stát vydavatele periodika

GB - Spojené království Velké Británie a Severního Irska

Počet stran výsledku

11

Strana od-do

1172-1182

Kód UT WoS článku

000929468100001

EID výsledku v databázi Scopus

2-s2.0-85147952629