GEOCHEMICAL
CHARACTERISTICS OF OLIVINES FROM
NORTHEASTERN
PHU QUY VOLCANIC ISLAND AND THEIR RELATION TO MELT VARIATIONS
IN THE MAGMA SOURCE
Le Duc Anh1,3,
Nguyen Hoang2,3, Phung Van Phach 1,3,
Malinovskii A,I4 ,
Dinh
Quang Sang5, Shakirov R,B6
1 Institute of Marine Geology and
Geophysics, VAST, Hanoi, Vietnam
2 Institute of
Geological Sciences, VAST, Hanoi, Vietnam
3 Graduate University
of Science and Technology
4 Federal State Budgetary Institution of
Science Far East Geological Institute, Far Eastern Branch of Russian Academy of
Sciences, Vladivostok, Russia
5 South Vietnam Geological Mapping Division, Ho Chi Minh, Viet Nam
6 V.I. Il’ichev Pacific Oceanological
Institute (POI), Far Eastern Branch of Russian Academy of Sciences,
Vladivostok, Russia
Corresponding
author: leducanh010282@gmail.com
Abstract: Phu Quy volcanic island is
formed following at least two major volcanic eruptions at ca. 2.64 Ma and 1.32
Ma. The early episode appeared as fissure eruptions producing a shield-like basement
comprising of tholeiitic basalt to sub-alkaline (olivine basalt). The later
episode occurred as monogenic volcanic, explosive eruption producing mainly
sub-alkaline basalt with a minor amount of (mantle xenolith- bearing) alkaline
basalt. Olivine phenocrysts and single crystals were separated from,
respectively, basalt and volcanic tuff to analyze for chemical compositions
with aim to understand the nature of mantle source region and melt generation
and evolution. The chemical compositions of olivine revealed that Phu Quy
magmatic melt was generated by mantle peridotite melting at a depth of about 90
km. Regardless of volcanic occurrence at two separate periods the continuity
between high – low melting pressure- produced melts may reflect melt mixing via
column melting. After generation, melt of the early eruption episode (2.64 Ma)
moved up to a depth of about 35 km before erupting. The later melt moved
directly to the surface from the segregation source. At a shallow depth (about
40-45 km) the melt partially mixed with melt of the early phase. This happened
may be due to the intrusion of asthenospheric flows from beneath, the
consequence of the Neo-Tethys ocean closure following the India-Eurasian
collision, causing the mantle temperature to rise, making melting easier to
form Phu Quy volcanic island.
Keywords: East Vietnam Sea,
Phu Quy Island, olivine chemistry, mantle extrusion, column melting.
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