日本地球惑星科学連合2019年大会

講演情報

[E] ポスター発表

セッション記号 S (固体地球科学) » S-CG 固体地球科学複合領域・一般

[S-CG49] ハードロック掘削科学~陸上掘削から深海底掘削、そしてオマーン~

2019年5月28日(火) 15:30 〜 17:00 ポスター会場 (幕張メッセ国際展示場 8ホール)

コンビーナ:道林 克禎(名古屋大学大学院環境学研究科地球環境科学専攻地質・地球生物学講座岩石鉱物学研究室)、高澤 栄一(新潟大学理学部地質科学科)、秋澤 紀克(東京大学 大気海洋研究所 海洋底科学部門)

[SCG49-P09] X-ray CT images of oceanic lithologies obtained on Oman Drilling Project drillcores during ChikyuOman 2017 and 2018

*道林 克禎1Kelemen Peter2Godard Margurette3高澤 栄一4Teagle Damon5The Oman Drilling Project Science Party6 (1.名古屋大学理学部地球惑星科学科、2.コロンビア大学、3.モンペリエ大学、4.新潟大学、5.サウサンプトン大学、6.ICDP)

キーワード:OmanDP、XCT、image

The Oman Drilling Project (OmanDP) has drilled >3,200 meters of the Oman ophiolite during Phases 1 and 2 in Holes GT1A, GT2A, GT3A, BT1B, CM1A, CM2B, BA1B, BA3A and BA4A. All cores have been described on board D/V Chikyu during the summers of 2017 and 2018. X-ray computed tomography (X-ray CT) images were obtained on all cores as a routine part of the IODP measurement protocol onboard D/V Chikyu.



The X-ray CT scanner (Discovery CT 750HD, GE Medical Systems) scans and reconstructs an image of a 1.4 m section in 10 minutes and produces a series of scan images, each 0.625 mm thick. The X-ray source and detector are installed inside of the gantry opposite each other. The excitation voltage and current for X-ray tube are 140 kV and 100 mA, respectively. Core samples are scanned in the gantry with a scanning rate of 20 mm/sec. The distribution of attenuation values mapped to an individual slice comprises the raw data that are used for subsequent image processing. Successive two-dimensional (2D) slices of 512 x 512 pixels yield a representation of attenuation values in three-dimensional (3D) voxels of 512 x 512 by ~1600 in length. Data generated for each core consist of core-axis-normal planes (XY planes) of X-ray attenuation values with dimensions of 512 × 512 pixels in 9 cm × 9 cm cross-section, with a resolution of 0.176 mm/pixel.


As a consequence, we have >3,200 meters length of X-ray CT images from the dyke/gabbro transition zone to the gabbroic sequence to the mantle sequence to the basal thrust of the ophiolite. All X-ray CT images have been processed to match with individual photo images of the archive halves of the cores. The data are useful for assessing sample locations and quality. X-ray CT images can be used for 3D fabric analyses even after core has been cut in half and subsampled for other analyses.