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"},"keywords":[{"id":"a56c609f-1561-4216-adb0-fc937f323b42","keyword":"超重核幻数","originalKeyword":"超重核幻数"},{"id":"bc154b1b-0f42-4d6f-9e65-64cf1cf70b5f","keyword":"杨立铭方法","originalKeyword":"杨立铭方法"},{"id":"913e281b-2cf2-4469-99de-7758f327a0c2","keyword":"Thomas-Fermi近似","originalKeyword":"Thomas-Fermi近似"}],"language":"zh","publisherId":"yzhwlpl200001009","title":"用杨立铭方法估算大于126的幻数","volume":"17","year":"2000"},{"abstractinfo":"杨坪金矿床赋存于下古生界丹凤群大草坝组变火山—沉积建造中,金矿化严格受层间挤压破碎(片理化)带控制,赋矿岩性为蚀变的二云石英片岩、绢云母石英片岩、绿泥石英片岩等变质岩及黄铁矿化石英脉,金矿化受变质、构造及次生氧化三重作用控制.对杨坪金矿床的地质特征及控矿特征进行了系统的研究,总结了找矿标志,并指出了找矿方向.","authors":[{"authorName":"张银斗","id":"8764fff0-6afd-4f47-8cbb-a0bc3aebc5e3","originalAuthorName":"张银斗"}],"doi":"","fpage":"24","id":"7c98a968-7112-4917-9271-e00b77970427","issue":"1","journal":{"abbrevTitle":"HJ","coverImgSrc":"journal/img/cover/HJ.jpg","id":"44","issnPpub":"1001-1277","publisherId":"HJ","title":"黄金"},"keywords":[{"id":"5034aee0-cb40-4bd0-b883-2eb1d15eac4b","keyword":"地质特征","originalKeyword":"地质特征"},{"id":"5f6b6235-c284-4a52-a713-e0bb3ac50aa3","keyword":"控矿特征","originalKeyword":"控矿特征"},{"id":"1e4733d3-52c3-4c63-9072-ff2e17cf002e","keyword":"找矿标志","originalKeyword":"找矿标志"},{"id":"f0b2ed2b-45f9-4bad-aba9-8b696a60102b","keyword":"找矿方向","originalKeyword":"找矿方向"},{"id":"abe0bc7e-b8e2-4095-a867-8c7cbb45a24f","keyword":"杨坪金矿床","originalKeyword":"杨坪金矿床"}],"language":"zh","publisherId":"huangj201301006","title":"甘肃杨坪金矿床控矿特征及找矿方向","volume":"","year":"2013"},{"abstractinfo":"杨砦峪金矿床为河南灵宝小秦岭地区一重要大型石英脉型金矿床,矿床空间产出受太华群变质地层、岩浆岩及断裂构造控制,层间断裂为主要容矿构造.矿脉内矿体产出表现出\"尖灭再现\"、\"尖灭侧现\"规律.综合研究表明,小秦岭地区金矿床深部具有存在第二矿化富集段的可能性,在杨砦峪矿区,矿脉东段深部仍存在较好的成矿远景和找矿潜力.","authors":[{"authorName":"张庆超","id":"bab17d0e-bafb-4b0d-a46c-af63e0f92041","originalAuthorName":"张庆超"}],"doi":"10.3969/j.issn.1001-1277.2004.10.006","fpage":"19","id":"a5e01dd1-9aa0-45a0-bbfc-dc367c2a13db","issue":"10","journal":{"abbrevTitle":"HJ","coverImgSrc":"journal/img/cover/HJ.jpg","id":"44","issnPpub":"1001-1277","publisherId":"HJ","title":"黄金"},"keywords":[{"id":"96b81f72-8929-4e32-a794-35b0f3908133","keyword":"杨砦峪金矿床","originalKeyword":"杨砦峪金矿床"},{"id":"6027da23-6ddc-4696-b051-89c13227848a","keyword":"石英脉型","originalKeyword":"石英脉型"},{"id":"0cb416f8-b21f-4ff8-b599-e31978de5af7","keyword":"地质特征","originalKeyword":"地质特征"},{"id":"1379a96f-cb9d-492f-9621-dd980419d399","keyword":"深部成矿远景","originalKeyword":"深部成矿远景"}],"language":"zh","publisherId":"huangj200410006","title":"杨砦峪金矿床地质特征及深部成矿远景评价","volume":"25","year":"2004"},{"abstractinfo":"本文研究了应用稀土保水剂对干旱地区新疆杨育苗的效应,结果表明:应用稀土保水剂能极大地提高苗木成活率,加速苗木的生长发育,根系数量、株高、地茎等生长量指标均明显高于对照.因此,应用稀土保水剂对育苗的成功率、培育壮苗都有一定的作用.","authors":[{"authorName":"王永刚","id":"38361a45-f110-4aeb-a580-2436cf6c6956","originalAuthorName":"王永刚"},{"authorName":"张宇生","id":"083931f0-09cd-4490-8ade-f310257d5949","originalAuthorName":"张宇生"},{"authorName":"张宏江","id":"22614210-1ed9-46b4-94f5-e83cfbf53d69","originalAuthorName":"张宏江"}],"doi":"10.3969/j.issn.1004-0277.2000.05.011","fpage":"38","id":"f2fb53ae-860a-4080-930b-25c1c781692f","issue":"5","journal":{"abbrevTitle":"XT","coverImgSrc":"journal/img/cover/XT.jpg","id":"65","issnPpub":"1004-0277","publisherId":"XT","title":"稀土"},"keywords":[{"id":"d6121fd6-2f0c-4b38-8415-0809dff7b660","keyword":"稀土保水剂","originalKeyword":"稀土保水剂"},{"id":"dbb6825d-5ea8-42fb-a3b7-faaa66286cd7","keyword":"育苗","originalKeyword":"育苗"},{"id":"5354a5b7-84ad-4b44-90af-4de66e718826","keyword":"成活率","originalKeyword":"成活率"},{"id":"9145b6d2-c58c-44ca-9db8-3924c802ab04","keyword":"生长量","originalKeyword":"生长量"}],"language":"zh","publisherId":"xitu200005011","title":"稀土保水剂在新疆杨育苗上的应用研究","volume":"21","year":"2000"},{"abstractinfo":"在野外调研基础上,通过对杨金沟金矿床地质特征的研究和包裹体显微测温的分析,讨论了成矿条件和矿床成因.结果表明,该矿床赋存于古生代变质岩系与华力西晚期花岗岩接触带附近,明显受断裂构造控制;金矿石主要有蚀变岩型和石英脉型两种,金矿物以细粒—微细粒的包体金、裂隙金和晶隙金形式赋存于石英、黄铁矿等矿物的内部、晶隙或裂隙中;石英中主要发育气液二相包裹体、C02包裹体和含C02三相包裹体,成矿流体为中温(230 ~ 270℃)、中低盐度(3.37%~15.65%)、低密度(0.78~0.91 g/cm3)的NaCl-H20-C02体系.结合区内铜金矿床对比分析认为,杨金沟金矿床形成于板块俯冲后的伸展环境,金矿化与燕山晚期中酸性侵入体具有密切的时空和成因联系.","authors":[{"authorName":"李晨辉","id":"5aea53a0-c9be-4402-aa16-7b76b92ab973","originalAuthorName":"李晨辉"}],"doi":"10.3969/j.issn.1001-1277.2011.12.006","fpage":"22","id":"0c921024-5b83-4ee5-b2b4-93a29adc8a04","issue":"12","journal":{"abbrevTitle":"HJ","coverImgSrc":"journal/img/cover/HJ.jpg","id":"44","issnPpub":"1001-1277","publisherId":"HJ","title":"黄金"},"keywords":[{"id":"bf599b86-a5f3-4782-bb4b-6986f6aaf40d","keyword":"地质特征","originalKeyword":"地质特征"},{"id":"c704fbcb-90a4-4649-a013-d2fe792bc4ce","keyword":"流体包裹体","originalKeyword":"流体包裹体"},{"id":"497fe4ae-5730-4e04-ac5f-eb6eeb134b40","keyword":"杨金沟金矿床","originalKeyword":"杨金沟金矿床"},{"id":"e917f097-ebf6-46f6-9148-a8da63819178","keyword":"延边东部地区","originalKeyword":"延边东部地区"}],"language":"zh","publisherId":"huangj201112006","title":"延边东部杨金沟金矿床地质特征与成矿物理化学条件研究","volume":"32","year":"2011"},{"abstractinfo":"","authors":[],"doi":"","fpage":"","id":"50cb3b82-505d-40eb-88fd-0d51cedd10fb","issue":"1","journal":{"abbrevTitle":"YZHWLPL","coverImgSrc":"journal/img/cover/YZHWLPL.jpg","id":"78","issnPpub":"1007-4627","publisherId":"YZHWLPL","title":"原子核物理评论 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