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| 1 | 柴达木盆地北缘大柴旦地区古生代花岗岩锆石SHRIMP定年显示文摘大柴旦地区是柴北缘古生代超高压带的重要组成部分,与超高压岩石相伴的花岗岩十分发育。这些花岗岩具有两类不同的岩石地球化学特征,Ⅰ类以 Na_2O/K_2O 比值小于1、明显的负 Eu 异常和低 Sr、高 Y 为特征,具有 S-型花岗岩的属性,Ⅱ类以 Na_2O/K_2O 比值大于1、弱负 Eu 异常到正 Eu 异常和高 Sr、低 Y 为特征,具有Ⅰ-型花岗岩的属性,反映了它们的源岩及成因上的差异。锆石 SHRIMP U—Ph 定年结果表明,大柴旦地区花岗岩的年龄可分为三组,第一组年龄为446.3±3.9Ma,第二组年龄分别为408.6±4.4Ma、403.3±3.8Ma、401.8±3Ma,第三组年龄分别为374.5±1.6Ma、372±2.1Ma。结合区域地质特征,我们认为,第一组年龄可能反映了柴达木陆块与中南祁连板块碰撞的时代,第二组年龄可能反映了深俯冲地下的板块由于拆沉而折返的时代,第三组年龄可能反映了碰撞隆起后造山带上不同块体之间的伸展、滑塌的时代。 | 吴才来 郜源红 吴锁平 陈其龙 Joseph L.WOODEN Frank K.MAZADAB Chris MATTINSON | 2007 | 岩石学报2007，23，8： | 88 |
| 2 | 柴北缘西段花岗岩锆石SHRIMP U-Pb定年及其岩石地球化学特征显示文摘柴北缘西段出露的花岗岩主要有赛什腾山、团鱼山、嗷唠河和三岔沟等岩体,这些岩体的走向为北西向,与区域构造线方向基本一致.岩体的锆石SHRIMP U—Pb定年结果表明,它们的时代从早古生代的奥陶纪到晚古生代的泥盆纪和二叠纪.其中,赛什腾山岩体为(465.4±3.5)Ma,团鱼山岩体两期侵入岩的年龄分别为(469.7±4.6)和(443.5±3.6)Ma;它们均属早古生代奥陶纪;而嗷唠河岩体的石英闪长岩为(372.1±2.6)Ma,属晚古生代泥盆纪;三岔沟岩体也由两期侵入岩组成,其年龄分别为(271.2±1.5)和(260.4±2.3)Ma,属二叠纪.花岗岩的岩石地球化学特征表明,柴北缘早古生代花岗岩具有岛弧或活动大陆边缘花岗岩的属性,原岩可能为中元古代(1.03~1.15Ga)形成的、来源于亏损地幔的拉斑玄武质洋壳,它们的形成与板块的俯冲作用有关;晚古生代花岗岩继承了早古生代花岗岩的特点,其原岩可能为中元古代(1.18—1.29Ga)的岛弧根部下地壳,岩浆物质成分以壳幔混合源为主,它们的形成与造山隆起后不同块体之间的均衡调整有关. | 吴才来 郜源红 吴锁平 陈其龙 JosephL.Wooden FrankK.Mazadab Chris Mattinson | 2008 | 中国科学(D辑)2008，38，8： | 89 |
| 3 | 铜陵狮子山地区中酸性侵入岩锆石SHRIMP U-Pb定年及岩浆作用的深部过程显示文摘铜陵狮子山地区中酸性侵入岩锆石 SHRIMP U-Pb 定年结果表明,白茫山辉石二长闪长岩、鸡冠山和大团山石英二长闪长岩以及胡村花岗闪长岩的年龄分别为:138.21±0.82Ma、139.9±1.1Ma、139.3±1.2Ma 和140.9±1.2Ma。岩浆侵位顺序为花岗闪长岩→石英二长闪长岩→辉石二长闪长岩。根据锆石 SHRIMP U-Pb 年龄变化范围,推测该区岩浆活动持续的时间约为15Ma,且岩浆属脉动式多次侵位,后期岩浆侵位的热使早期岩体中已结晶的锆石发生熔解、重结晶,形成新的锆石。地下深部岩浆活动频繁,形成了多级岩浆房,使得本区的莫霍面界线不明显。 | 吴才来 董树文 国和平 郭祥炎 高前明 刘良根 陈其龙 雷敏 WOODENJ L MAZADAB FK MATTINSON C | 2008 | 岩石学报2008，24，8： | 62 |
| 4 | 柴达木北缘榴辉岩中的柯石英及其意义显示文摘柯石英是超高压变质作用的直接标志.柴北缘副片麻岩的锆石中已报道有柯石英包体的存在,但在榴辉岩中还没有发现柯石英保存.通过详细的岩相学观察和拉曼光谱的测定,在柴北缘阿尔茨托山(都兰超高压变质单元南带)的榴辉岩中发现柯石英,这些柯石英在石榴子石中呈包体分布,部分被具有栅状结构的石英替代.这是柴北缘地区首次在榴辉岩中发现柯石英,也与榴辉岩670~730℃和2.7~3.25GPa的温压估算相符合.除柴北缘都兰超高压单元之外,柴北缘其他单元的榴辉岩及相关岩石中还没有发现柯石英及其假象,是否柴北缘普遍经历过超高压变质作用还需进一步研究. | 张建新 孟繁聪 李金平 Mattinson C. G. | 2009 | 科学通报2009，54，5： | 40 |
| 5 | Geochemistry and zircon SHRIMP U-Pb dating of granitoids from the west segment of the North Qaidam显示文摘Granitoid intrusives such as Saishitenshan, Tuanyushan, Aolaohe and Sanchagou occur widely in the western segment of North Qaidam. All these bodies trend NW, roughly parallel to the regional structure. Zircon SHRIMP dating for these granites show that they range in age from Ordovician to Permian; 465.4±3.5 Ma for Saishitenshan, 469.7±4.6 Ma and 443.5±3.6 Ma for Tuanyushan, 372.1±2.6 Ma for Aolaohe, and 271.2±1.5 Ma and 259.9±1.2 Ma for Sanchagou. Both the Tuanyshan and Aolaohe plutons record two distinct intrusive events. Geochemically, the early Paleozoic granites have an island arc or active continental margin affinity, and their protolith may have been Mesoproterozoic oceanic crust derived from depleted mantle. The protolith of the late Paleozoic granites may have been Mesoproterozoic lower crust from the root of an island arc with the magmas reflecting a mixture of mantle and crustal material. | Joseph L.WOODEN Paul T.ROBINSON Frank K.MAZDAB Chris MATTINSON | 2009 | Science China Earth Sciences2009，52，11： | 16 |
| 6 | Coesite in eclogite from the North Qaidam Mountains and its implications显示文摘Coesite provides direct evidence for ultrahigh pressure metamorphism. Although coesite has been found as inclusions in zircon in paragneiss of the north Qaidam Mountains, it has never been identified in eclogite. In this contribution, based on petrographic observations and in situ Raman microprobe spectroscopy, coesite was identified as inclusions in garnet of eclogite from the Aercituoshan, Dulan UHP metamorphic unit, north Qaidam Mountains. Coesite is partly replaced by quartz, showing a pali-sade texture. This is the first report on coesite in eclogite from the north Qaidam Mountains, and is also supported by garnet-omphacite-phengite geothermobarometry (2.7―3.25 GPa, 670―730℃). Coesite and its pseudomorphs have not been found in eclogites and associated rocks of other units of the north Qaidam Mountains. Further studies are required to confirm if all metamorphic units in the north Qaidam Mountains underwent the ultrahigh-pressure metamorphism. | ZHANG JianXin MENG FanCong LI JinPing MATTINSON C.G. | 2009 | Chinese Science Bulletin2009，54，6： | 14 |
| 7 | Alginate coatings for preservation of minimally processed ‘Gala’ apples显示文摘 | G.I. Olivas D.S. Mattinson G.V. Barbosa-Cánovas | 2007 | Postharvest Biology and Technology2007，，1： | 2 |
| 8 | Two contrasting eclogite cooling histories, North Qaidam HP/UHP terrane, western China:Petrological and isotopic constraints显示文摘 | Zhang J X Yang J S Mattinson C G | 2005 | Lithos2005，84，： | 1 |
| 9 | Two contrasting eclogite cooling histories,North Qaidam HP/UHP terrane,western China:Petrological and isotopic constraints显示文摘 | Zhang J X Yang J S Mattinson C G Xu Z Q | 2005 | Lithos2005，84，： | 1 |
| 10 | Quality retention in strawberry and carrot purees dried with Refractance Window^TM System显示文摘 | ABONYI B l FENG H TANG J EDWARDS C G CHEW B P MATTINSON D S FELLMAN J K | 2001 | Jour- nal of Food Science2001，67，： | 1 |
| 11 | Alginate coatings for preservation of minimally processed ‘Gala' apples 显示文摘 | Olivas GI Mattinson DS Barbosa- Canovas GV | 2007 | Postharvest Biology and Technology2007，45，1： | 1 |
| 12 | Alginate coatings for preservation of minimally processed Gala apples显示文摘 | Olivas G I Mattinson D S Barbosa-Cánovas G V | 2007 | Postharvest Biol Tec2007，45，1： | 1 |
| 13 | Interaction of TiO2 Nano-Particles with Organic UV Absorbers显示文摘 | Egerton T Everall N Mattinson J | 2008 | Journal of Photochemistry & Photobiology A:Chemistry2008，193，1： | 1 |
| 14 | The influence of platinum on UV and visible photocatalysis by rutile and degussa P25显示文摘 | Egert on T A Mattinson J A | 2008 | Phot ochemistry and Photobiology A: Chemistry2008，194，23： | 1 |
| 15 | Effects of ethanol,tannin and fructose on the headspace concentration and potential sensory significance of odorants in a model wine显示文摘 | VILLAMOR R R EVANS M A MATTINSON D S | 2013 | Food Research International2013，50，1： | 1 |
| 16 | Factors that influence biosynthesis of volatile flavor compounds in apple fruits显示文摘 | Fellman J K Miller T W Mattinson D S | 2000 | HortScience2000，35，6： | 1 |
| 17 | Two contrasting eclogite cooling histories,North Qaidam HP/UHP terrane,western China:Petrological and isotopic constraints显示文摘 | ZhangJ X Yang J S Mattinson C G | | 0，，1： | 1 |
| 18 | Factors that influence biosynthesis of volatile flavor compounds in apple fruits 显示文摘 | Fellman J K Miller T W Mattinson D S | 2000 | Hort Science2000，35，6： | 1 |
| 19 | Alginate coatings for preservation of minimally pro-cessed‘Gala’apples显示文摘 | Olivas G I Mattinson D S Barbosa-C'anovas G V | 2007 | Postharvest Biology and Tech-nology2007，45，： | 1 |
| 20 | Analysis of volatile compounds from various types of barley cultivars显示文摘 | Cramer A C J Mattinson D S Fellman J K | 2005 | Journal of Agricultural and Food Chemistry2005，53，75： | 1 |
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