臺灣西南海域永安海脊冷泉址沉積物之反差性黃鐵礦組織

Translated title of the contribution: Contrasting pyrite textures in sediments from a cold-seep site at Yung-An Ridge, offshore southwestern Taiwan

Ta-Wei Hsu, Wei-Teh Jiang

Research output: Contribution to journalArticle

Abstract

A record of temporal cold-seep activities associated with enhanced anaerobic oxidation of methane in the Yung-An Ridge sediments offshore southwestern Taiwan was marked by the occurrence of high pyrite concentrations and local formation of carbonate nodules in sediments from the upper and lower sections of long piston core MD052911. Electron microscopic analysis of the cored sediments indicate that pyrite has a variety of microtextures including framboidal and irregular aggregates of fine-grained crystals, patches of disseminated anhedral to euhedral grains, and anhedral grains enclosed within microfissures of phyllosilicate cleavage. In addition, high percentages of pyrite framboids showing prominent overgrowth and pyrite neoformation within pellets of ferric smectite occur in these sediments. These diversified pyrite growth textures can occur in a single specimen and have no systematic correlation with burial depth. These imply subtle differences in geochemical environment over short distances, in accordance with a migration mode of methane dominated by slow seepage and/or diffusion. In contrast, the middle-section sediments contain much smaller amounts of pyrite with scanty framboidal aggregates and anhedral grains due to a lack of intense anaerobic oxidation of methane.
Original languageChinese
Pages (from-to)8-25
Number of pages18
JournalThe Taiwan Mining Industry
Volume67
Issue number2
Publication statusPublished - 2015 Jun

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cold seep
pyrite
texture
sediment
methane
oxidation
phyllosilicate
smectite
cleavage
seepage
crystal
carbonate
electron

All Science Journal Classification (ASJC) codes

  • Earth and Planetary Sciences(all)

Cite this

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title = "臺灣西南海域永安海脊冷泉址沉積物之反差性黃鐵礦組織",
abstract = "A record of temporal cold-seep activities associated with enhanced anaerobic oxidation of methane in the Yung-An Ridge sediments offshore southwestern Taiwan was marked by the occurrence of high pyrite concentrations and local formation of carbonate nodules in sediments from the upper and lower sections of long piston core MD052911. Electron microscopic analysis of the cored sediments indicate that pyrite has a variety of microtextures including framboidal and irregular aggregates of fine-grained crystals, patches of disseminated anhedral to euhedral grains, and anhedral grains enclosed within microfissures of phyllosilicate cleavage. In addition, high percentages of pyrite framboids showing prominent overgrowth and pyrite neoformation within pellets of ferric smectite occur in these sediments. These diversified pyrite growth textures can occur in a single specimen and have no systematic correlation with burial depth. These imply subtle differences in geochemical environment over short distances, in accordance with a migration mode of methane dominated by slow seepage and/or diffusion. In contrast, the middle-section sediments contain much smaller amounts of pyrite with scanty framboidal aggregates and anhedral grains due to a lack of intense anaerobic oxidation of methane.",
author = "Ta-Wei Hsu and Wei-Teh Jiang",
year = "2015",
month = "6",
language = "Chinese",
volume = "67",
pages = "8--25",
journal = "The Taiwan Mining Industry",
number = "2",

}

臺灣西南海域永安海脊冷泉址沉積物之反差性黃鐵礦組織. / Hsu, Ta-Wei; Jiang, Wei-Teh.

In: The Taiwan Mining Industry, Vol. 67, No. 2, 06.2015, p. 8-25.

Research output: Contribution to journalArticle

TY - JOUR

T1 - 臺灣西南海域永安海脊冷泉址沉積物之反差性黃鐵礦組織

AU - Hsu, Ta-Wei

AU - Jiang, Wei-Teh

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Y1 - 2015/6

N2 - A record of temporal cold-seep activities associated with enhanced anaerobic oxidation of methane in the Yung-An Ridge sediments offshore southwestern Taiwan was marked by the occurrence of high pyrite concentrations and local formation of carbonate nodules in sediments from the upper and lower sections of long piston core MD052911. Electron microscopic analysis of the cored sediments indicate that pyrite has a variety of microtextures including framboidal and irregular aggregates of fine-grained crystals, patches of disseminated anhedral to euhedral grains, and anhedral grains enclosed within microfissures of phyllosilicate cleavage. In addition, high percentages of pyrite framboids showing prominent overgrowth and pyrite neoformation within pellets of ferric smectite occur in these sediments. These diversified pyrite growth textures can occur in a single specimen and have no systematic correlation with burial depth. These imply subtle differences in geochemical environment over short distances, in accordance with a migration mode of methane dominated by slow seepage and/or diffusion. In contrast, the middle-section sediments contain much smaller amounts of pyrite with scanty framboidal aggregates and anhedral grains due to a lack of intense anaerobic oxidation of methane.

AB - A record of temporal cold-seep activities associated with enhanced anaerobic oxidation of methane in the Yung-An Ridge sediments offshore southwestern Taiwan was marked by the occurrence of high pyrite concentrations and local formation of carbonate nodules in sediments from the upper and lower sections of long piston core MD052911. Electron microscopic analysis of the cored sediments indicate that pyrite has a variety of microtextures including framboidal and irregular aggregates of fine-grained crystals, patches of disseminated anhedral to euhedral grains, and anhedral grains enclosed within microfissures of phyllosilicate cleavage. In addition, high percentages of pyrite framboids showing prominent overgrowth and pyrite neoformation within pellets of ferric smectite occur in these sediments. These diversified pyrite growth textures can occur in a single specimen and have no systematic correlation with burial depth. These imply subtle differences in geochemical environment over short distances, in accordance with a migration mode of methane dominated by slow seepage and/or diffusion. In contrast, the middle-section sediments contain much smaller amounts of pyrite with scanty framboidal aggregates and anhedral grains due to a lack of intense anaerobic oxidation of methane.

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