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188篇 您的检索式:作者名="Dill H"
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1西藏多龙矿集区热构造演化历史——来自磷灰石(U-Th)/He的证据显示文摘西藏多龙矿集区是西藏最重要的斑岩-浅成低温热液型矿集区。多龙矿集区经历了多期次的构造抬升-剥蚀事件,成矿后的埋藏-剥蚀历史对矿体的保存至关重要。本文运用磷灰石(U-Th)/He数据对多龙矿集区的低温热年代学进行研究。磷灰石(U-Th)/He年龄平均值分布在85. 1±4. 0Ma到37. 9±2. 5Ma,记录了晚白垩世到古新世、始新世、渐新世的热-构造事件。热历史模拟显示,多龙矿集区主要经历4次冷却事件:Ⅰ) 100~75Ma,冷却速率约为4℃/Myr,剥速率约为0. 16km/Myr,与班公湖-怒江洋的闭合以及拉萨-羌塘地块的碰撞事件有关;Ⅱ) 75~45Ma,冷却速率约为0. 3℃/Myr,剥蚀速率约为0. 01km/Myr,与拉萨-羌塘地块的继续碰撞事件以及由碰撞作用引起的逆冲推覆构造事件有关;Ⅲ) 45~30Ma,冷却速率约为2℃/Myr,剥蚀速率约为0. 08km/Myr,与印度-欧亚大陆的碰撞抬升事件有关;Ⅳ) 30Ma至今,冷却速率约为1℃/Myr,剥蚀速率约为0. 04km/Myr,与渐新世以来印度-欧亚大陆的持续碰撞作用以及渐新世以来青藏高原发育的频繁构造事件有关。多龙矿集区斑岩-浅成低温热液型矿床形成后在强烈的隆升-剥蚀的环境下保存下来,得益于早白垩世美日切错组火山岩的覆盖,由拉萨-羌塘地块碰撞作用引起的逆冲推覆构造引起的上部地层加厚,以及印度-欧亚大陆碰撞事件在多龙矿集区产生的相对较弱的破坏效应。拉萨-羌塘地块碰撞作用引起的地层加厚对多龙矿集区矿床起主要的保护作用。杨欢欢 宋扬 DILLES John H SOUSA Francis DANI?íK Martin 杨超 2019岩石学报2019,35,3:4
2Physical performance in relation to external temperature显示文摘Dill D B Edwards H T Bauer P S 1931Aebeitsphysiol1931,4,:1
3Rapamycin causes poorly reversible inhibition of roTOR and induces p53-independent apoptosis in human rhabdomyosarcoma cells 显示文摘Hosoi H Dilling MB Shikata T 1999Cancer Res1999,59,4:1
4Intrachain loops in polymers:effects of excluded volume显示文摘Chan H S Dill K A 0,,:1
5The 'chessboard' classification scheme of mineral deposits : Mineralogy and geology from aluminum to zirconium 显示文摘Dill H G 2010Earth- S cience Reviews2010,100,:1
6Optical lithography显示文摘F H Dill 1975IEEE Trans Electron Devices1975,22,7:1
7Intronic miR-26b controls neuronal differentiation by repressing its host tran-script,etdsp2显示文摘Dill H Linder B Fehr A 2012Genes Dev2012,26,1:1
8The'chessboard'classification scheme of mineral deposits:Mineralogy and geology from aluminum to zirconium显示文摘Dill H G 2010Earth-Science Reviews2010,100,1:1
9Porphyry deposits: Characteristics and origin of hypogene {eatures显示文摘SEEDORFF E DILLES J H PROFFETT J M 2005Economic Geology2005,100,:1
10Characterization of positive photoresist显示文摘F H Dill W P Hornberger P S Hauge 1975IEEE Trans Electron Devices1975,22,7:1
11The 'chessboard' classification scheme of mineral depos- its: Mineralogy and geology from aluminum to zirconium显示文摘Dill H G 2010Earth- Science Reviews2010,100,14:1
12Bisphenol A:acute aquatic toxity 显示文摘Alexander H Dill D Smith L 1988Environ Toxicol Chem1988,7,:1
13Sulfur evolution of oxidized are magmas as recorded in apatite from a porphyry copper batholiths 显示文摘Streck J M Dilles J H 1998Geology1998,26,:1
14Traction characteristics of high-temperatare powder-lubricated ceramics ( si3 n4/alpha-sic) 显示文摘Heshmat H S Dill J F 1992Tribology Transactions1992,35,2:1
15Stabilization of proteins in confined spaces显示文摘Zhou H X Dill KA 2001Biochemistry2001,40,11:1
16Characterization of positive photoresist显示文摘DILL F H HORNBERGER W P HAUGE P S 1975Electron Devices1975,22,7:1
17Fluid inclusion evidence for magmatic-hydrothermal fluid evolution in the porphyry copper-molybdenum deposit at Butte, Montana显示文摘Rusk B G Reed M H Dilles J H 2008Economic Geology2008,103,2:1
18Interferoninduced gene expres- sion is a stronger predictor of treatment response than IL28B genotype in patients with hepatitis C 显示文摘Dill M T Duong F H Vogt J E 2011Gastroenterology2011,140,:1
19Repressing a repressor: gibberellin-induced rapid reduction of the RGA protein in Arabidopsis 显示文摘Silverstone A L Jung H S Dill A 2001Plant Cell2001,13,:1
20Dynamics of Rolling-Element Bearings Experimental Validation of the DREB and RAPIDREB Computer Programs 显示文摘Gupta P K Dill J F Bandow H E 1985Journal of Tribology1985,107,:1
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