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| 1 | 北祁连早古生代花岗质岩浆作用及构造演化显示文摘北祁连山中段花岗岩锆石SHRIMP定年结果表明,柯柯里岩体的斜长花岗岩和石英闪长岩的年龄分别为512Ma和501 Ma,野马咀和金佛寺花岗岩的年龄分别为508Ma和424Ma。结合区内其它花岗岩体的定年资料,根据花岗岩的岩石地球化学特征及岩体产出的构造位置、区域地质资料等,我们认为,早古生代北祁连洋板块向南俯冲,至少引发了两期花岗质岩浆作用,第一次岩浆作用形成柯柯里斜长花岗岩(512Ma)、野马咀花岗岩(508Ma)和柯柯里石英闪长岩(501 Ma),第二次花岗质岩浆作用形成牛心山花岗岩(477Ma)。由于往南俯冲的板块受到柴达木板块向北俯冲的影响,俯冲受阻,继而俯冲极性发生变化,转向北俯冲,形成了民乐窑沟(463Ma)等花岗岩侵入体。大约440Ma之后,洋盆闭合,柴达木陆块和阿拉善陆块对接碰撞,形成北祁连造山带。由于造山带根部岩石圈发生折沉作用,造山带上不同的块体伸展、滑塌,形成一系列碰撞后花岗岩如金佛寺花岗岩(424Ma)及牛心山岩体的石英闪长岩(435Ma)等。 | 吴才来 徐学义 高前明 李向民 雷敏 郜源红 Ronald B FROST Joseph L WOODEN | 2010 | 岩石学报2010，26，4： | 132 |
| 2 | 北阿尔金地区米兰红柳沟蛇绿岩的岩石学特征和SHRIMP定年显示文摘米兰红柳沟蛇绿岩是北阿尔金蛇绿岩带中发育和保留最好的蛇绿岩,主要由地幔橄榄岩、镁铁-超镁铁质堆晶杂岩、岩墙群和基性熔岩等组成。它们以规模不等的构造岩块产出,大者长十余km,宽近1km,组成一条近100km长的蛇绿混杂岩带。地幔橄榄岩以方辉橄榄岩为主,有少量纯橄岩,主要由橄榄石(Fo=91.2~92.7),斜方辉石(En=93~98)和少量单斜辉石(En=46)组成;副矿物尖晶石Cr^#为43~69(平均55),Mg^#为43~64(平均58),表现出深海橄榄岩(Abyssal peridotite)和俯冲带环境(SSZ)橄榄岩成分特点。深成堆晶岩主要由异剥橄榄岩-橄榄二辉石岩-(橄榄)辉石岩-辉长岩-斜长岩,该组合的堆晶岩通常被认为是SSZ构造背景的产物。席状岩墙群的岩石成分与熔岩一致,其TiO2(1%~1.5%)和低含量的K2O〈0.3%和P2O5表明具有MORB型的岩石特征,并得到了不相容元素和LREE平坦型和亏损型的球粒陨石标准化模型等证据的支持。该地区另存在一套高Ti的洋岛型拉斑玄武岩。两类熔岩的存在,以及地幔橄榄岩和堆晶岩的不同特征,表明米兰红柳沟蛇绿岩组合可能来自不同构造背景。带中与洋壳俯冲有关的蓝片岩和榴辉岩组成的高压变质带的存在,以及与俯冲碰撞有关的不同类型花岗岩类的产出,表明米兰红柳沟蛇绿混杂岩带代表了一个复杂的板块缝合带。蛇绿岩中辉长岩的锆石SHRIMP年代为479±8Ma,这是获得的第一个北阿尔金蛇绿岩的锆石SHRIMP U—Pb同位素年龄,认为代表蛇绿岩的形成时代。因此。北阿尔金缝合带无论在年龄和特征等方面,均可以与阿尔金断裂带东部的北祁连缝合带对比,证实两个带曾经是一个带,被阿尔金断裂左旋错断了约400km。 | 杨经绥 史仁灯 吴才来 苏德辰 陈松永 王希斌 WOODEN Joseph | 2008 | 岩石学报2008，24，7： | 115 |
| 3 | 北祁连洋早古生代双向俯冲的花岗岩证据显示文摘笔者主要对北祁连山中段的牛心山岩体、民乐窑沟岩体进行了锆石SHRIMP定年研究。结果表明:牛心山花岗岩的年龄为476 Ma,民乐窑沟花岗闪长岩的年龄为463 Ma。岩石地球化学显示,两岩体均具有大陆活动边缘的岩浆作用特征,结合岩体产出的区域构造位置及区域地质资料,笔者认为早古生代北祁连洋板块分别发生了向南、向北俯冲,其中向南俯冲形成牛心山花岗岩(476 Ma),向北俯冲,形成了民乐窑沟花岗岩侵入体(463 Ma)。 | 吴才来 姚尚志 杨经绥 曾令森 陈松永 李海兵 戚学祥 Joseph L. Wooden Frank K.Mazdab | 2006 | 中国地质2006，33，6： | 80 |
| 4 | 南阿尔金茫崖地区花岗岩类锆石SHRIMP U-Pb定年、Lu-Hf同位素特征及岩石成因显示文摘南阿尔金茫崖地区早古生代花岗岩锆石SHRIMP U-Pb定年结果表明,阿克提山花岗岩为264±1Ma,柴水沟花岗岩分别为404±5Ma、406±4Ma,其中的辉绿岩为454±4Ma,常春沟花岗岩分别为411±5Ma、406±3Ma,茫崖镇北石英闪长岩为466±5Ma,阿卡龙山花岗岩为469±6Ma。锆石Lu-Hf同位素分析表明,εHf(t)值大多数为正值,少数继承性锆石为负值,反映了它们的源岩以新生地壳为主,同时,也混有少量的古大陆壳的成分。结合区域地质特征和各岩体的岩石地球化学特征,将南阿尔金茫崖地区早古生代花岗质岩浆活动划分为3期,第一期(465~469Ma)岩石组合为石英闪长岩+花岗闪长岩+花岗岩,具有岛弧火成岩的地球化学属性,其形成可能与洋壳的俯冲作用有关;第二期(404~411Ma)岩石组合为花岗闪长岩+二长花岗岩+正长花岗岩,具有A型花岗岩的地球化学特征,可能与板块碰撞后造山带块体均衡调整有关,第三期(264Ma)岩石组合为石英闪长岩+二长花岗岩+正长花岗岩,也具有I型花岗岩的特征,可能与阿尔金断裂的活动有关。 | 吴才来 郜源红 雷敏 秦海鹏 刘春花 李名则 B Ronald FROST Joseph L WOODEN | 2014 | 岩石学报2014，30，8： | 56 |
| 5 | 都兰花岗岩锆石SHRIMP定年及柴北缘超高压带花岗岩年代学格架显示文摘柴北缘超高压带东端都兰地区花岗岩锆石SHRIMP U-Pb定年结果表明,野马滩东岩体的年龄为(406.6±3.5)Ma,巴立给哈滩西岩体的年龄分别为(407.3±4.3)和(397±6)Ma,水文站北岩体的年龄分别为(404.5±4.0)和(397.0±3.7)Ma,水文站南岩体的年龄为(380.5±5.0)Ma,察察公麻岩体的年龄分别为(382.5±3.6)和(372.5±2.8)Ma.从年龄上看,这些花岗岩明显地分为两期:早期的为407-397 Ma,晚期的为383-373 Ma.它们主要为准铝质-弱过铝质的石英闪长岩、花岗闪长岩和二长花岗岩.岩石地球化学研究表明,大多数样品为钙碱性系列,少数样品为钙性或碱钙性系列,其中,早期花岗岩的87Sr/86Sr比值(0.7082-0.7110)和模式年龄(T2DM=1.41-1.90 Ga)高于晚期花岗岩(0.7072-0.7091,T2DM=1.07-1.38 Ga),但晚期花岗岩的εNd(t)值(0.6- -3.0)高于早期花岗岩(-3.2- -9.3),表明早期花岗岩可能起源于早中元古代的大陆壳;而晚期花岗岩起源于晚中元古代玄武质地壳.结合区域地质构造特征,可以认为,早期花岗岩的形成与俯冲板块的断离并折返有关,而晚期花岗岩的形成与造山带岩石圈地幔拆沉作用有关. | 吴才来 郜源红 李兆丽 雷敏 秦海鹏 李名则 刘春花 Ronald B FROST Paul T ROBINSON Joseph L WOODEN | 2014 | 中国科学:地球科学2014，44，10： | 27 |
| 6 | Zircon SHRIMP U-Pb dating of granites from Dulan and the chronological framework of the North Qaidam UHP belt, NW China显示文摘Zircon SHRIMP dating of granites from Dulan,east segment of North Qaidam UHP belt shows that they are 406.6±3.5 Ma for Yematan-E,407.3±4.3 and 397±6 Ma for Balijiehatan-W,404.5±4.0 and 397.0±3.7 Ma for Shuiwenzhan-N,380.5±5.0 Ma for Shuiwenzhan-S,382.5±3.6 and 372.5±2.8 Ma for Chachagongma.These granites from Dulan represent the products of the third and fourth periods of Paleozoic magmatism in North Qaidam.Geochemically,the granitoids with metalumious to weak peratuminous are quartz diorite,granodiorite,and granite in composition and mainly belong to calc-alkaline series,a few samples to calc or alkali-calc series.The third period of granites is a rock association of granodiorite+granite,with initial 87Sr/86Sr ratios from 0.7082 to 0.7110 and T2DM model ages from 1.41–1.90 Ga;and the fourth period of granites is a rock association of quartz diorite+granodiorite+granite,with initial 87Sr/86Sr ratios from 0.7072 to 0.7091 and T2DM model ages from 1.07–1.38 Ga.Therefore,the third period of granites has higher initial 87Sr/86Sr ratios and T2DM model ages.On the contrary,the fourth period of granites has Nd(t)values from 0.6 to-3.0,higher than that of the third granite with Nd(t)values-3.2 to-9.3.Thus,the data comparison indicates that the third granites may derive from Paleo-proterzoic continental crust with mantle material whereas the fourth granites may derive from the Meso-proterzoic basalt crust with continental material.Combined with regional geology,we thought that the third granites were formed relative to plate exhumation and the fourth granites to delamination of the lithospheric mantle. | WU CaiLai GAO YuanHong LI ZhaoLi LEI Min QIN HaiPeng LI MinZe LIU ChunHua Ronald B FROST Paul T ROBINSON Joseph L WOODEN | 2014 | Science China Earth Sciences2014，57，12： | 21 |
| 7 | Bashikaogong-Shimierbulake granitic complex, north Altun, NW China:Geochemistry and zircon SHRIMP ages显示文摘The Bashikaogong-Shimierbulake granitoid complex is about 30 km long and 2―6 km wide, with an area of 140 km2, located at the north margin of the Bashikaogong Basin in the north Altun terrain. It intruded into schist, metapelite and metatuff of Precambrian ages. This granitoid complex consists of darkish quartz diorite, grey granite, pink granite and pegmatite. Geochemically, the quartz diorite has I-type granite affinity and belongs to Calc-alkaline sereies, and the other gran- ites have S-type affinity and to high-K calc-alkaline series. Zircon SHRIMP U-Pb dating shows that the quartz diorite has a bigger age than those of other granites, which is 481.6±5.6 Ma for quartz diorite, 437.0±3.0 Ma―433.1±3.4 Ma for grey granite and 443±11 Ma―434.6±1.6 Ma for pink granite, re- spectively. Combined with regional geology, we think that the quartz diorite formed in tectonic envi- ronment related to oceanic crust subduction and the granites in post-collision. | Joseph L. Wooden Frank K. Mazdab | 2006 | Science China Earth Sciences2006，49，12： | 4 |
| 8 | Trace element composition of igneous zircon: a thermal and compositional record of the accumulation and evolution of a large silicic batholith, Spirit Mountain, Nevada显示文摘 | Lily L. Claiborne Calvin F. Miller Joseph L. Wooden | 2010 | Contributions to Mineralogy and Petrology2010，，4： | 1 |
| 9 | Origin of Sr, Nd and Pb isotopic systematics in high-Sr basalts from central Arizona显示文摘 | James H. Wittke Douglas Smith Joseph L. Wooden | 1989 | Contributions to Mineralogy and Petrology1989，，1： | 1 |
| 10 | SHRIMP U-Pb Zircon Dating of the Tula Granite Pluton on the South Side of the Altun Fault and Its Geological Implications显示文摘摘要:Tula A2 子类型花岗石 pluton 在 Altun 差错和它的分叉的差错之间被定位。根据地质, geochemical, REE 和踪迹元素特征,它属于 A2 (PA ) 子类型花岗石。标明日期的虾 U-Pb 锆石给 385.2 | WU Suoping WU Cailai WANG Meiying CHEN Qilong Joseph L. WOODEN | 2008 | Acta Geologica Sinica(English Edition)2008，82，2： | 1 |
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