

FOLLOWUS
1.Key Laboratory of Ocean Observation and Forecasting and Key Laboratory of Marine Geology and Environment, Institute of Oceanology, Chinese Academy of Sciences, Qingdao266071, China
2.Laboratory for Marine Geology, Qingdao Marine Science and Technology Center, Qingdao266237, China
3.University of Chinese Academy of Sciences, Beijing100049, China
4.Institute of Marine Chemistry and Environment, Ocean College, Zhejiang University, Zhoushan316021, China
5.College of Marine Technology and Environment, Dalian Ocean University, Dalian116023, China
6.Key Laboratory of Marine Sedimentology and Environmental Geology, First Institute of Oceanography, Ministry of Natural Resources, Qingdao266061, China
fqjiang@qdio.ac.cn
zhaohui_zhang@zju.edu.cn
Received:06 September 2023,
Online First:09 January 2024,
Published:01 September 2024
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JIANG Fuqing,ZHANG Zhishun,ZHANG Zhaohui,et al.Provenance of colorless and brown volcanic glass in late Pleistocene tephra layers in the Western Philippine Sea[J].Journal of Oceanology and Limnology,2024,42(05):1438-1449.
JIANG Fuqing,ZHANG Zhishun,ZHANG Zhaohui,et al.Provenance of colorless and brown volcanic glass in late Pleistocene tephra layers in the Western Philippine Sea[J].Journal of Oceanology and Limnology,2024,42(05):1438-1449. DOI: 10.1007/s00343-024-3182-1.
Tephra layers in the western Philippine Sea
characterized by abundant volcanic glass shards
may provide crucial evidence on the eruption history of volcanoes and tectonic evolution of the western Pacific. A 220-ka sediment core from the Benham Rise in the western Philippine Sea offers new insights into the provenance of four intercalated tephra layers (T1–T4
in chronological order) containing either colorless or brown glass shards. Relative to primitive mantle
all glass shards are enriched in large-ion lithophile elements
such as Rb
Cs
and Pb
and depleted in high field-strength elements
such as Th
Nb
and Ta
indicating a subduction-related origin. The colorless glass shards are characterized by high SiO
2
(
>
78%) and light rare earth element (LREE) contents as well as high La/Sm ratios (
>
9)
low FeO and MgO contents (
<
1%)
low Sr/Y (
<
15) and high Ba/Th ratios (
>
100)
pointing to a rhyolitic composition and a medium-K calc-alkaline serial affinity. In contrast
the brown glass shards are characterized by lower SiO
2
(
<
63%) and LREE contents
higher FeO
MgO
and CaO contents
lower La/Sm (
<
6) and Ba/Th (
<
75)
and similar Sr/Y ratios (
<
15)
indicating derivation from medium to high-K calc-alkaline andesite magma. Brown glass shards from layers T3 (152 ka) and T4 (172 ka) were correlated with volcanic deposits from the Taal and Laguna Caldera in the Maccolod Corridor
respectively
while the colorless glass shards from layers T1 (36.5 ka) and T2 (61.2 ka) were likely sou
rced from the Irosin Caldera in the Bicol Arc. Establishing the provenance of late Pleistocene tephra layers in the western Philippine Sea is helpful to complement a Philippine volcanic history and establish a regional tephro-chronostratigraphy.
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