{"id":"8455d100-6557-4cf7-b5e3-11fc47fa65f5","title":"池州地区铜钼多金属花岗闪长岩（斑岩）形成的地球动力学演化模式简述图","title_en":"Geodynamic evolution model of Cu-Mo polymetallic granodiorite (porphyry) in the Chizhou area","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":"数据以jpg形式储存，无文件命名方式。使用方法：将数据通过有图片编辑器功能软件打开即可。","description":"数据内容包括：对池州地区铜钼多金属花岗闪长岩（斑岩）形成的地球动力学演化模式简述。图中分别画出150Ma之前及150Ma之后在池州地区地质构造发生的变化，以及对成矿模式的影响方式变化。池州地区150 Ma时受到古太平洋板块倒转的影响，形成无海洋沉积物的弧内裂谷环境。板块释放的流体使地幔楔体物质熔融，产生了高氧逸度环境，形成了富氯流体和混合的幔壳岩浆，促进了金属的提取和运移，最终形成了池州地区的铜钼多金属矿床。\n以上数据已发表于SCI高级别期刊，数据真实可靠。数据以jpg格式储存。","doi":"doi.org/10.1016/j.oregeorev.2019.04.018","projection":"","language":"zh","share_type":"online","east":117.67,"west":117.33,"south":30.33,"north":30.67,"scale":null,"crs":null,"filesize":0.59,"share_policy":"a","ts_created":"2021-05-18T16:08:59.404411+08:00","doi_type":"沿用数据已有DOI","ts_updated":"2021-05-24T09:36:34.176911+08:00","time_description":"150Ma","datas_group":3,"time_description_en":"150Ma","data_format":null,"project":[11],"specials":[],"cite":null,"review_status":5,"review_invite":[{"user_name":"颜茂都","username":"颜茂都","email":"maoduyan@itpcas.ac.cn","is_cancel_expert":true}],"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":"8455d100-6557-4cf7-b5e3-11fc47fa65f5","three_pole":null,"third_pole":null},"username":"谢建成","review_time":null,"protected_duration":null,"protected_describe":null,"is_important":false,"hit_count":451}