Japan Geoscience Union Meeting 2015

Presentation information


Symbol B (Biogeosciences) » B-CG Complex & General

[B-CG28] Interrelation between Life, Water, Mineral, and Atmosphere

Tue. May 26, 2015 6:15 PM - 7:30 PM Convention Hall (2F)

Convener:*Fumito Shiraishi(Department of Earth and Planetary Systems Science, Graduate School of Science, Hiroshima University), Tsubasa Otake(Division of Sustainable Resources Engineering, Faculty of Engineering, Hokkaido University), Yohey Suzuki(Graduate School of Science, The University of Tokyo), Ken Takai(Extremobiosphere Research Center, Japan Agency for Marine-Earth Science & Technology), Yuichiro Ueno(Department of Earth and Planetary Sciences, Tokyo Institute of Technology), Takeshi Naganuma(Graduate School of Biosphere Science), Takeshi Kakegawa(Graduate School of Science, Tohoku University), Tadashi Yokoyama(Department of Earth and Space Science, Graduate School of Science, Osaka University), Kentaro Nakamura(Precambrian Ecosystem Laboratory (PEL), Japan Agency for Marine-Earth Science and Technology (JAMSTEC))

6:15 PM - 7:30 PM

[BCG28-P08] Mobilization of manganese and iron in marine sediments and tuffs by dolerite in Hokuroku Distirict.

*Yuya TSUKAMOTO1, Takeshi KAKEGAWA1 (1.Graduate School of Science, Tohoku University)

Keywords:banded manganese deposit, Hokuroku district, Kuroko, hydrothermal activity, redox state

Mn rich sediments are often used to evaluate the presence of submarine hydrothermal activities and the redox state of paleoenvironment in the sea. The oldest Mn ore deposit occurs 2.4 billion years ago as the banded manganese formation, corresponded to oxidation of Precambrian ocean water. Those studies suggest that Mn geochemistry is important to consider not only the Earth history but also paleoenvironment evaluation.
Hokuroku distirict is famous for Kuroko deposits which is rich in metals such as Zn, Cu, and Pb. During the hydrothermal activities, metals of forming Kuroko precipitated in closed area around ores, on the other hand Mn and Fe can be transported in distal by hydrothermal plume, as a result of formation of Mn and Fe rich sediments on the Kuroko horizon without heavy metal deposition. Therefore,the first purpose of this research is to evaluate the exploration potential of Kuroko deposits using Mn, thus the examination of spatial relationship between Mn and Kuroko ores. Presence of Mn rich layers is also known in the Hokuroku district. Their origin was completely unknown. Mn rich layers were potentially formed submarine hydrothermal activities related post Kuroko ore forming activities. Therefore, the second purpose of this research is to discuss whether the submarine hydrothermal activity was present even after Kuroko ore formation and if they are responsible for Mn enrichment in post Kuroko mudstone.
I have investigated the ”M2” mudstone which is often overlaid with Kuroko deposits. For the first purposes, 6 Samples of ”M2” mudstones were collected from 3 areas. Moreover, I have investigated the Mn rich layer to discuss the second purpose. 31 Samples of ”R2”,”T2”, dolerite, and mudstone were collected from Koyukizawa areas. The mineral and chemical compositions of the samples were examined by standard petrographic microscopy, SEM,and EPMA. Chemical composition of samples were determined by energy dispersive X-ray spectrometry, and EDXRF. Mineral assemblage is determined by X-ray diffraction (XRD).
For the first purpose, Mn concentrations in ”M2” mudstones are found to be about 0.04 wt%, which is low concentrations. I can’t find the change of Mn concentrations according to the distance from ores. Therefore, it suggested that Mn is not the exploration index of Kuroko deposits at this stage. For the second purpose, the geological survey was performed in the area of Koyukizawa (route A and route B). Tuff breccia and pumice tuff are abundant in this area associated with mudstones. Those were intruded by dolerite. Red to brown alteration are common even in dolerite representing hydrothermal alterations in route A. I could find the Mn rich layers(3.7 wt%, 1.8 wt%) by chemical analyses. Partial Mn enrichments were also found in rocks on the boundary between ”T2” and dolerite. On the other hand, I can’t find the red alteration in dolerite route B. From those findings, Mn rich layer was formed by the recycle of Mn by heat generated from the intruding dolerite. Mn was enriched in rocks when circulated hydrothermal water was oxic enough. Moreover, by EDXRF, Mn and Fe have similar behavior, and Mn was oxidized prior to Fe on the oxidative environment.