Suhendro, Indranova and Bunga Naen, Gabriela Nogo Retnaningtyas and Gurusinga, Andriansyah and Sari, Sistien Adhaena and Moktikanana, Mradipta Lintang Alifcanta and Gunawan, Rachmi Mustika Pertiwi Putri and Jane, Jesslyn and Qodri, Muhammad Fatih and Sya'bana, Faraz and Cahyani, Sherinna Mega and Ardian, Dini Nuari (2023) Dynamics of the Young Merapi (<2.2 ka – 1,788 CE) pumice fall deposits: Insights from textural and geochemical studies. Journal of Volcanology and Geothermal Research, 443. ISSN 03770273
1-s2.0-S0377027323001762-main.pdf - Published Version
Restricted to Registered users only
Download (27MB) | Request a copy
Abstract
We studied nine pumice fall deposits of the Young Merapi stage (<2.2 ka – 1,788 CE) observed in the western and southern flanks of Merapi volcano. All deposits include a wide variation of lithics (10–42 Clithic), with thicker deposits (i.e., more voluminous eruption) being more lithic-rich and vice versa. Two different magma types (hereafter referred to as type I and type II) were identified based on petrography, bulk-rock, glass, and feldspar microlite compositions. Type I magma has abundant amphibole and pyroxene, is rich in calcium (>9 wt CaObulk), poor in both silica (50.8–53.7 wt SiO2 bulkand 62.3–66.6 wt SiO2 glass) and strontium (<580 ppm, bulk-rock), and has more calcic feldspar microlites (An38 – 79). Type II magma also contains abundant amphibole, but has less pyroxene and is poorer in calcium (<9 wt CaObulk), higher in both silica (53.2–54.5 wt SiO2 bulk and 63.3–70.8 wt SiO2 glass) and strontium (>580 ppm), with less calcic feldspar microlites (An31 – 77). These two magma types alternately fed the explosive eruptions during the Young Merapi stage; however, their juvenile products are distinctive in terms of syn-eruptive microtextures (i.e., matrix-vesicles and microlites). Pumices from type II magma have a higher matrix-vesicle number density (MVND) and microlite number density (MND) values than those of pumices from type I magma (1.0–6.5 × 1015 and 1.8–7.4 × 1015 m−3, and 0.6–2.3 × 1015 and 0.7–1.8 × 1015 m−3, respectively). A positive correlation between MVND with SiO2 and MND suggests that a colder (i.e., less calcic feldspar microlites indicate lower temperature and vice versa) and more evolved (higher SiO2) magma facilitates more extensive matrix-bubble nucleation and deeper microlite crystallization than hotter magmas, allowing type II magma to erupt more explosively than type I magma. © 2023
Item Type: | Article |
---|---|
Additional Information: | Cited by: 3 |
Uncontrolled Keywords: | East Java; Greater Sunda Islands; Java; Merapi; Sunda Isles; Calcium; Deposits; Feldspar; Glass; Matrix algebra; Strontium; Volcanoes; Decompression rate; Magma decompression rate; Merapi volcanos; Microlite number density; Microlites; Number density; Pumouse fall deposit; Type II; Vesicle number density; Young merapi; geochemistry; magma; pumice; texture; vesicle; volcanology; Silica |
Subjects: | G Geography. Anthropology. Recreation > G Geography (General) G Geography. Anthropology. Recreation > GB Physical geography |
Divisions: | Faculty of Geography > Departemen Geografi Lingkungan |
Depositing User: | Sri Purwaningsih Purwaningsih |
Date Deposited: | 03 Sep 2024 01:27 |
Last Modified: | 03 Sep 2024 01:27 |
URI: | https://ir.lib.ugm.ac.id/id/eprint/6123 |