{"id":"2d431daa-6396-4a5c-965f-cd652dc9a183","title":"乌拉斯沟铜矿床S-Pb-Sr-Nd-C-H-O数据","title_en":"S-pb-sr-nd-c-h-o data of Wulasigou copper deposit","serial":"","user_limit":"为尊重知识产权、保障数据作者的权益、扩展数据中心的服务、评估数据的应用潜力，请数据使用者在使用数据所产生的研究成果中（包括公开发表的论文、论著、数据产品和未公开发表的研究报告、数据产品等成果），明确注明数据来源和数据作者。对于转载（二次或多次发布）的数据，作者还须注明原始数据来源。","instructions":"乌拉斯沟铜矿床S-Pb-Sr-Nd-C-H-O数据以Excel的格式存储，文件的名称为“Wlsgshocsrndpb.xlsl”。其中Wlsg代表乌拉斯沟铜矿床，s代表硫同位素，ho代表氢-氧同位素，c代表碳同位素，sr代表锶同位素，nd代表钕同位素，pb代表铅同位素","description":"新疆乌拉斯沟铜矿床位于阿尔泰造山带南缘克兰盆地内，为近年来新发现的矿床，受 ＮＷ 向断裂控制的脉状矿体产于 泥盆系康布铁堡组变质火山岩系中，目前其成矿流体和成矿物质来源尚不明确，在细致的矿床地质研究基础上，通过开展S-Pb-Sr-Nd-C-Ｈ-Ｏ同位素分析，根据野外和显微镜下观察，可将乌拉斯沟铜矿床的形成划分为黄铁矿－磁铁矿－石英、黄铜矿－绿泥石－绿帘石－石英及石英－碳酸盐阶段。通过S、Sr-Nd-Pd同位素的分析，发现成矿物质来源可能源自康布铁堡组，且受外来流体影响。对C-H-O同位素分析可进一步解释成矿流体来源。","doi":"10.3799/dgkx.2018.135","projection":"","language":"zh","share_type":"protected","east":91.0,"west":86.0,"south":46.0,"north":49.0,"scale":null,"crs":null,"filesize":0.023,"share_policy":"a","ts_created":"2021-05-27T10:39:18.697390+08:00","doi_type":"沿用数据已有DOI","ts_updated":"2021-05-31T23:13:41.128275+08:00","time_description":"晚古生代","datas_group":0,"time_description_en":"Late Paleozoic","data_format":null,"project":[11],"specials":[],"cite":null,"review_status":5,"review_invite":[{"user_name":"王浩","username":"王浩_iggcas","email":"wanghao@mail.iggcas.ac.cn","is_cancel_expert":false}],"review_editor":{"id":42421,"last_login":"2022-04-08T15:16:51.670544+08:00","username":"任慧霞","email":"510727846@qq.com","is_active":true,"is_staff":true,"user_name":"任慧霞"},"data_sources":null,"temporal_resolution":"1000 year < x","spatial_resolution":"1km - 10km","license":"Attribution-NonCommercial-ShareAlike 4.0 International (CC BY-NC-SA 4.0)","fund":[521],"subtopics":{"metadata":"2d431daa-6396-4a5c-965f-cd652dc9a183","three_pole":null,"third_pole":null},"username":"龙丽洁","review_time":null,"protected_duration":24,"protected_describe":null,"is_important":false,"hit_count":357}