首页|The Calatrava paradox to decipher the origin of carbonatites: A petrological insight on Finca La Nava, Calatrava Province (central Spain)

The Calatrava paradox to decipher the origin of carbonatites: A petrological insight on Finca La Nava, Calatrava Province (central Spain)

扫码查看
The paper presents a detailed petrographic and geochemical study of the pyroclastites outcropping at La Nava maar (Calatrava Volcanic Province-CVP). Here, extrusive carbonatites mix with melilite nephelinite lapilli and bombs, crustal and mantle debris. Nephelinite and carbonatite are not characterised by a HFSE distribution typical of immiscible pairs. IREE and La/Lu ratios reflect primitive mantle carbonates and kimberlites. Igneous carbonates have 613C and 6180 isotopic ratios in the range of extrusive carbonatites and differ from local sedimentary carbonates. Carbonatites have 87Sr/86Sr and 144Nd/143Nd isotopic ratios similar to Calatrava leucitites but different to melilite nephelinite. The difference indicates that melilite nephelinites and carbonatites are co-eruptive but not comagmatic. The mingled magmatic convoy, underwent decarbonation processes, releasing Ca and Mg that reacted with parental silicate melt. Consequently, the nephelinitic melt evolved towards a melilititic composition producing Ca-rich overgrowths on mafic phenocrysts and reacted to produce high Mg#, low Cr + Ni forsterite. Mass balance calculations indicats that the nephelinite magma assimilated up to 30% of the carbonatite magma. Mixing modelling based on the Sr and Nd isotopic composition of mantle xenoliths and carbonatites indicate that La Nava carbonatite may represent the mantle metasomatic agent.

Carbonatite-nepheliniteMinglingDecarbonatationSilicate carbonate reactionMantle metasomatismCalatrava Volcanic Province

G. Rosatelli、E. Humphreys-Williams、F. Wall

展开 >

Department of Psychology, Health and Territory Sciences, G. d'Annunzio University of Chieti-Pescara, Via dei Vestmi 31, 06100 Chieti, Italy

Natural History Museum, London SW7 5BD, UK

Camborne School of Mines, University of Exeter, Penryn Campus, Cornwall TR10 9FE, UK

2022

Lithos

Lithos

SCI
ISSN:0024-4937
年,卷(期):2022.416/417
  • 5
  • 81