Mineralogical and geochemical characteristics of hydrothermal minerals collected from hydrothermal vent ffields in the Southern Mariana spreading center

Kei Ikehata, Ryohei Suzuki, Kazuhiko Shimada, Jun Ichiro Ishibashi, Tetsuro Urabe

Research output: Chapter in Book/Report/Conference proceedingChapter

4 Citations (Scopus)

Abstract

Archaean and Pika sites) in the Southern Mariana Trough was investigated to clarify the mineralogical and geochemical characteristics of the hydrothermal minerals. The Snail site and the Yamanaka site are located on the crest of the backarc spreading ridge (on-axis). The Pika site sits atop an off-axial volcano, 4.9 km distant from the spreading axis, while the Archaean site sits on the flank of the spreading ridge, about 1.5 km distant from the axis. In the four hydrothermal sites, chimney and mound sulfides are composed mainly of pyrite, marcasite, sphalerite and chalcopyrite. Conduits and interstices of these sulfide minerals are filled with late barite and anhydrite. Mineralizations of off-axial hydrothermal fields have mineralogical and geochemical signatures (Fe-rich and low fS2 condition) similar to those of mineralizations at sediment-free mid-ocean ridge settings. By contrast, mineralizations of on-axial sites show distinctly Zn and Pb-rich (high fS2 condition) signatures similar to those found in arc or rifting settings. Sulfur isotopic compositions of collected sulfide minerals show a similar diversity with a mid-ocean ridge range for the off-axial sites and an island-arc range for the on-axial sites. These isotopic signatures could be explained by varying proportions of magmatic sulfur leached from the underlying volcanic rocks and reduced seawater sulfates.

Original languageEnglish
Title of host publicationSubseafloor Biosphere Linked to Hydrothermal Systems
Subtitle of host publicationTAIGA Concept
PublisherSpringer Japan
Pages275-288
Number of pages14
ISBN (Electronic)9784431548652
ISBN (Print)9784431548645
DOIs
Publication statusPublished - Jan 1 2015

Fingerprint

hydrothermal vent
spreading center
sulfide
mid-ocean ridge
mineralization
Archean
mineral
sulfur
marcasite
barite
anhydrite
sphalerite
chalcopyrite
snail
rifting
island arc
pyrite
volcanic rock
trough
isotopic composition

All Science Journal Classification (ASJC) codes

  • Earth and Planetary Sciences(all)

Cite this

Ikehata, K., Suzuki, R., Shimada, K., Ishibashi, J. I., & Urabe, T. (2015). Mineralogical and geochemical characteristics of hydrothermal minerals collected from hydrothermal vent ffields in the Southern Mariana spreading center. In Subseafloor Biosphere Linked to Hydrothermal Systems: TAIGA Concept (pp. 275-288). Springer Japan. https://doi.org/10.1007/978-4-431-54865-2_22

Mineralogical and geochemical characteristics of hydrothermal minerals collected from hydrothermal vent ffields in the Southern Mariana spreading center. / Ikehata, Kei; Suzuki, Ryohei; Shimada, Kazuhiko; Ishibashi, Jun Ichiro; Urabe, Tetsuro.

Subseafloor Biosphere Linked to Hydrothermal Systems: TAIGA Concept. Springer Japan, 2015. p. 275-288.

Research output: Chapter in Book/Report/Conference proceedingChapter

Ikehata, K, Suzuki, R, Shimada, K, Ishibashi, JI & Urabe, T 2015, Mineralogical and geochemical characteristics of hydrothermal minerals collected from hydrothermal vent ffields in the Southern Mariana spreading center. in Subseafloor Biosphere Linked to Hydrothermal Systems: TAIGA Concept. Springer Japan, pp. 275-288. https://doi.org/10.1007/978-4-431-54865-2_22
Ikehata K, Suzuki R, Shimada K, Ishibashi JI, Urabe T. Mineralogical and geochemical characteristics of hydrothermal minerals collected from hydrothermal vent ffields in the Southern Mariana spreading center. In Subseafloor Biosphere Linked to Hydrothermal Systems: TAIGA Concept. Springer Japan. 2015. p. 275-288 https://doi.org/10.1007/978-4-431-54865-2_22
Ikehata, Kei ; Suzuki, Ryohei ; Shimada, Kazuhiko ; Ishibashi, Jun Ichiro ; Urabe, Tetsuro. / Mineralogical and geochemical characteristics of hydrothermal minerals collected from hydrothermal vent ffields in the Southern Mariana spreading center. Subseafloor Biosphere Linked to Hydrothermal Systems: TAIGA Concept. Springer Japan, 2015. pp. 275-288
@inbook{cdd6eaf0182f40a7953ef1d96ac77b39,
title = "Mineralogical and geochemical characteristics of hydrothermal minerals collected from hydrothermal vent ffields in the Southern Mariana spreading center",
abstract = "Archaean and Pika sites) in the Southern Mariana Trough was investigated to clarify the mineralogical and geochemical characteristics of the hydrothermal minerals. The Snail site and the Yamanaka site are located on the crest of the backarc spreading ridge (on-axis). The Pika site sits atop an off-axial volcano, 4.9 km distant from the spreading axis, while the Archaean site sits on the flank of the spreading ridge, about 1.5 km distant from the axis. In the four hydrothermal sites, chimney and mound sulfides are composed mainly of pyrite, marcasite, sphalerite and chalcopyrite. Conduits and interstices of these sulfide minerals are filled with late barite and anhydrite. Mineralizations of off-axial hydrothermal fields have mineralogical and geochemical signatures (Fe-rich and low fS2 condition) similar to those of mineralizations at sediment-free mid-ocean ridge settings. By contrast, mineralizations of on-axial sites show distinctly Zn and Pb-rich (high fS2 condition) signatures similar to those found in arc or rifting settings. Sulfur isotopic compositions of collected sulfide minerals show a similar diversity with a mid-ocean ridge range for the off-axial sites and an island-arc range for the on-axial sites. These isotopic signatures could be explained by varying proportions of magmatic sulfur leached from the underlying volcanic rocks and reduced seawater sulfates.",
author = "Kei Ikehata and Ryohei Suzuki and Kazuhiko Shimada and Ishibashi, {Jun Ichiro} and Tetsuro Urabe",
year = "2015",
month = "1",
day = "1",
doi = "10.1007/978-4-431-54865-2_22",
language = "English",
isbn = "9784431548645",
pages = "275--288",
booktitle = "Subseafloor Biosphere Linked to Hydrothermal Systems",
publisher = "Springer Japan",
address = "Japan",

}

TY - CHAP

T1 - Mineralogical and geochemical characteristics of hydrothermal minerals collected from hydrothermal vent ffields in the Southern Mariana spreading center

AU - Ikehata, Kei

AU - Suzuki, Ryohei

AU - Shimada, Kazuhiko

AU - Ishibashi, Jun Ichiro

AU - Urabe, Tetsuro

PY - 2015/1/1

Y1 - 2015/1/1

N2 - Archaean and Pika sites) in the Southern Mariana Trough was investigated to clarify the mineralogical and geochemical characteristics of the hydrothermal minerals. The Snail site and the Yamanaka site are located on the crest of the backarc spreading ridge (on-axis). The Pika site sits atop an off-axial volcano, 4.9 km distant from the spreading axis, while the Archaean site sits on the flank of the spreading ridge, about 1.5 km distant from the axis. In the four hydrothermal sites, chimney and mound sulfides are composed mainly of pyrite, marcasite, sphalerite and chalcopyrite. Conduits and interstices of these sulfide minerals are filled with late barite and anhydrite. Mineralizations of off-axial hydrothermal fields have mineralogical and geochemical signatures (Fe-rich and low fS2 condition) similar to those of mineralizations at sediment-free mid-ocean ridge settings. By contrast, mineralizations of on-axial sites show distinctly Zn and Pb-rich (high fS2 condition) signatures similar to those found in arc or rifting settings. Sulfur isotopic compositions of collected sulfide minerals show a similar diversity with a mid-ocean ridge range for the off-axial sites and an island-arc range for the on-axial sites. These isotopic signatures could be explained by varying proportions of magmatic sulfur leached from the underlying volcanic rocks and reduced seawater sulfates.

AB - Archaean and Pika sites) in the Southern Mariana Trough was investigated to clarify the mineralogical and geochemical characteristics of the hydrothermal minerals. The Snail site and the Yamanaka site are located on the crest of the backarc spreading ridge (on-axis). The Pika site sits atop an off-axial volcano, 4.9 km distant from the spreading axis, while the Archaean site sits on the flank of the spreading ridge, about 1.5 km distant from the axis. In the four hydrothermal sites, chimney and mound sulfides are composed mainly of pyrite, marcasite, sphalerite and chalcopyrite. Conduits and interstices of these sulfide minerals are filled with late barite and anhydrite. Mineralizations of off-axial hydrothermal fields have mineralogical and geochemical signatures (Fe-rich and low fS2 condition) similar to those of mineralizations at sediment-free mid-ocean ridge settings. By contrast, mineralizations of on-axial sites show distinctly Zn and Pb-rich (high fS2 condition) signatures similar to those found in arc or rifting settings. Sulfur isotopic compositions of collected sulfide minerals show a similar diversity with a mid-ocean ridge range for the off-axial sites and an island-arc range for the on-axial sites. These isotopic signatures could be explained by varying proportions of magmatic sulfur leached from the underlying volcanic rocks and reduced seawater sulfates.

UR - http://www.scopus.com/inward/record.url?scp=84944584549&partnerID=8YFLogxK

UR - http://www.scopus.com/inward/citedby.url?scp=84944584549&partnerID=8YFLogxK

U2 - 10.1007/978-4-431-54865-2_22

DO - 10.1007/978-4-431-54865-2_22

M3 - Chapter

AN - SCOPUS:84944584549

SN - 9784431548645

SP - 275

EP - 288

BT - Subseafloor Biosphere Linked to Hydrothermal Systems

PB - Springer Japan

ER -