{"_buckets": {"deposit": "2d6fb187-e691-4e3e-bffb-d2e34436b510"}, "_deposit": {"id": "16116", "owners": [], "pid": {"revision_id": 0, "type": "depid", "value": "16116"}, "status": "published"}, "_oai": {"id": "oai:nagoya.repo.nii.ac.jp:00016116"}, "item_9_alternative_title_19": {"attribute_name": "\u305d\u306e\u4ed6\u306e\u8a00\u8a9e\u306e\u30bf\u30a4\u30c8\u30eb", "attribute_value_mlt": [{"subitem_alternative_title": "Groundwater conducting fracture and fracture fillings in deep crystalline rock : An occurrence and formation process"}]}, "item_9_biblio_info_6": {"attribute_name": "\u66f8\u8a8c\u60c5\u5831", "attribute_value_mlt": [{"bibliographicIssueDates": {"bibliographicIssueDate": "2012-03", "bibliographicIssueDateType": "Issued"}, "bibliographicPageEnd": "56", "bibliographicPageStart": "54", "bibliographicVolumeNumber": "23", "bibliographic_titles": [{"bibliographic_title": "\u540d\u53e4\u5c4b\u5927\u5b66\u52a0\u901f\u5668\u8cea\u91cf\u5206\u6790\u8a08\u696d\u7e3e\u5831\u544a\u66f8"}]}]}, "item_9_description_4": {"attribute_name": "\u6284\u9332", "attribute_value_mlt": [{"subitem_description": "Fractures distributed in crystalline rock inevitably influence fluid transport and solute migration. Most evaluations of those fluid conducting features and contaminant migration processes have been conducted mainly by the present hydrological characteristic of fractures for deep underground usages (e.g., for high level radioactive waste (HLW) disposal, LPG and C02 storage). In the orogenic field of Japan, there are wide areas of crystalline rock. The rocks in each area have a distinctive history which is partly reflected in the characteristics of the fracture systems and associated mineral fillings that occur. The structural and mineralogical features readily illustrate how certain contaminants might react and be retarded by the fracture fillings and open pore geometry, due to chemical sorption and/or physical retardation. The work reported here seeks to provide geological evidence that natural long-term physical and chemical processes are unlikely to change the overall transport and retardation properties of the rock significantly. 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