Gravitational collapse of a volcano edifice as a trigger for explosive carbonatite eruption?

Result code in IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00025798%3A_____%2F24%3A10169058" target="_blank" >RIV/00025798:_____/24:10169058 - isvavai.cz</a>

Result on the web

<a href="https://doi.org/10.1130/B37013.1" target="_blank" >https://doi.org/10.1130/B37013.1</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.1130/B37013.1" target="_blank" >10.1130/B37013.1</a>

Result language

angličtina

Original language name

Gravitational collapse of a volcano edifice as a trigger for explosive carbonatite eruption?

Original language description

The Miocene Kaiserstuhl volcanic complex in the Rhine graben rift is known for simultaneously exposing both intrusive and erupted (pyroclastic) calciocarbonatites. This makes Kaiserstuhl a promising candidate for studying the field and genetic relations between intrusive calciocarbonatite and its eruptive equivalent, and the processes enabling eruption of the calciocarbonatite at the surface in particular. Eruptive calciocarbonatites in Kaiserstuhl are represented by carbonatite tuff and lapillistone beds covering a debrite fan on the western flank of the volcano. The debrites are interpreted as lahar (debris flow) and possibly also debris -avalanche deposits. Based on the observed textures, the debris flows were most likely derived by water dilution from debris avalanches resulting from edifice failure, which occurred in the central part of the Kaiserstuhl volcanic complex. The edifice failure ultimately exposed the intrusive system, and the carbonatite pyroclasts (lapilli and ash) were ejected from narrow vents represented by open -framework tuff-breccias aligned along the detachment scarp. Since the Ca -carbonates break down rapidly at high temperatures and low pressures, calciocarbonatites are unlikely to form surface lavas. On the other hand, the presence of the calciocarbonatite pyroclastic deposits suggests that some geological process faster than the high -temperature breakdown of Ca -carbonate may facilitate calciocarbonatite eruption. We suggest that the sudden ex posure and decompression of a suprasolidus high-level carbonatite intrusion by edifice collapse may be a suitable scenario enabling calciocarbonatite eruption. The absence of edifice failures on alkaline volcanoes, where carbonatite intrusion is either supposed or exposed, may explain the overall scarcity of erupted calciocarbonatites.

Czech name

—

Czech description

—

Type

J_imp - Article in a specialist periodical, which is included in the Web of Science database

CEP classification

—

OECD FORD branch

10507 - Volcanology

Project

<a href="/en/project/GX19-29124X" target="_blank" >GX19-29124X: EVOLUTION AND POST-EMPLACEMENT HISTORY OF CARBONATITES: IMPLICATIONS FOR THE MOBILITY AND CONCENTRATION OF CRITICAL METALS</a><br>

Continuities

P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)

Publication year

2024

Confidentiality

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

Name of the periodical

Geological Society of America Bulletin

ISSN

0016-7606

e-ISSN

1943-2674

Volume of the periodical

136

Issue of the periodical within the volume

5-6

Country of publishing house

US - UNITED STATES

Number of pages

14

Pages from-to

2291-2304

UT code for WoS article

001235269300006

EID of the result in the Scopus database

2-s2.0-85186358941