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| 1 | PBL:教育实践和研究的未来挑战显示文摘本文是一篇有关PBL的评论性研究,根据现代学习理论,作者论述了四个有关学习的原则,解释了这些原则在PBL中的应用,并对已进行的研究进行了评议。 | Diana HJM Dolmans Willem De Grave Ineke HAP Wolfhagen Cees PM van der Vleuten 梅人朗 | 2008 | 复旦教育论坛2008，6，1： | 44 |
| 2 | Exhuming the Meso-Cenozoic Kyrgyz Tianshan and Siberian Altai-Sayan:A review based on low-temperature thermochronology显示文摘Thermochronological datasets for the Kyrgyz Tianshan and Siberian Altai-Sayan within Central Asia reveal a punctuated exhumation history during the Meso-Cenozoic.In this paper,the datasets for both regions are collectively reviewed in order to speculate on the links between the Meso-Cenozoic exhumation of the continental Eurasian interior and the prevailing tectonic processes at the plate margins.Whereas most of the thermochronological data across both regions document late Jurassic-Cretaceous regional basement cooling,older landscape relics and dissecting fault zones throughout both regions preserve Triassic and Cenozoic events of rapid cooling,respectively.Triassic cooling is thought to reflect the Qjangtang- Eurasia collision and/or rifting/subsidence in the West Siberian basin.Alternatively,this cooling signal could be related with the terminal terrane-amalgamation of the Central Asian Orogenic Belt.For the Kygyz Tianshan,late Jurassic-Cretaceous regional exhumation and Cenozoic fault reactivations can be linked with specific tectonic events during the closure of the Palaeo-Tethys and Neo-Tethys Oceans,respectively.The effect of the progressive consumption of these oceans and the associated collisions of Cimmeria and India with Eurasia probably only had a minor effect on the exhumation of the Siberian Altai-Sayan.More likely,tectonic forces from the east(present-day coordinates) as a result of the building and collapse of the Mongol-Okhotsk orogen and rifting in the Baikal region shaped the current Siberian Altai-Sayan topography.Although many of these hypothesised links need to be tested further,they allow a first-order insight into the dynamic response and the stress propagation pathways from the Eurasian margin into the continental interior. | Stijn Glorie Johan De Grave | 2016 | Geoscience Frontiers2016，7，2： | 13 |
| 3 | Apatite-fission-track geochronology and its tectonic correlation in the Dabieshan orogen,central China显示文摘AFT data of granitoid and metamorphic samples from the Dabieshan orogen have an age range between 96.4 Ma and 41.9 Ma coupled with confined track lengths of 11.5—14.0 μm, reflecting the cooling time of rocks differentially through the 100℃± isotherm. The Juras- sic-Eogene sediments from the North Huaiyang and Hefei basin, however, yield their AFT ages of 128.8—62.0 Ma with mean track lengths of 8.6—11.9 μm, recording a complicated thermal de- velopment of the basin. These AFT data structurally allowing the coupling between the orogen and the basin are to a great extent considered as the result from the control of NNE-trending regional tectonics. It took place approximately at 95—90 Ma that the orogen developed with an abrupt shift from the doming extension to the differential transtension, which is assumed to be related with the changes of the convergence between the Western Pacific and Eurasia plates. The differentially sinistral strike-slipping from the transtension between Tanlu and Shang- cheng-Macheng faults brought the doming extension of the orogen shrunk sharply in Late Cre- taceous. In Eogene, the full-grown transtension that dominated in East Asia was caused mainly by a rapid decrease of the rates of the Western Pacific convergence, which can be therefore re- garded as a major mechanism creating the zonal anomalies of 60—40 Ma in the orogen. The thermal anomaly of 70—40 Ma zonally along the Tanlu fault cooled more slowly than the anomaly of 60—55 Ma zoning along the Shangcheng-Macheng fault, but the 60—40 Ma anomaly trending E-W in hinterlands of the orogen seems to be relicts of the doming extension as a result of inten- sive rebuilding by the transtension. In addition, the orogen was also reactivated by the far-field effect from India-Asia collision in Eogene, where major NWW-trending faults played an important role in facilitating such far-field tectonic transferring. In Oligocene to Miocene, the Dabieshan orogen remained a few thermal disturbances with their AFT ages particularly in coincidence with the time of opening and closing of the South China Sea. | P. Van Den Haute R. A. Donelick J. De Grave MA Changqian P. W. Reiners | 2005 | Science China Earth Sciences2005，48，4： | 9 |
| 4 | Meso-Cenozoic tectonic evolution of the Talas-Fergana region of the Kyrgyz Tien Shan revealed by low-temperature basement and detrital thermochronology显示文摘This study provides new low-temperature thermochronometric data, mainly apatite fission track data on the basement rocks in and adjacent to the Talas-Fergana Fault, in the Kyrgyz Tien Shan in the first place.In the second place, we also present new detrital apatite fission track data on the Meso-Cenozoic sediments from fault related basins and surrounding intramontane basins. Our results confirm multistaged Meso-Cenozoic tectonic activity, possibly induced by the accretion of the so-called Cimmerian blocks to the Eurasian margin. New evidence for this multi-staged thermo-tectonic activity is found in the data of both basement and Meso-Cenozoic sediment samples in or close to the Talas-Fergana Fault.Zircon(U-Th)/He and apatite fission track data constrain rapid Late TriassiceE arly Jurassic and Late JurassiceE arly Cretaceous basement cooling in the Kyrgyz Tien Shan around 200 Ma and 130 -100 Ma respectively. Detrital apatite fission track results indicate a different burial history on both sides of the Talas-Fergana Fault. The apatite fission track system of the Jurassic sediments in the Middle Tien Shan unit east of the Talas-Fergana Fault is not reset, while the Jurassic sediments in the Fergana Basin and Yarkand-Fergana Basin, west of the fault zone, are partially and in some cases even totally reset. The totally reset samples exhibit Oligocene and Miocene ages and evidence the Cenozoic reactivation of the western Kyrgyz Tien Shan as a consequence of the India-Eurasia convergence. | Simon Nachtergaele Elien De Pelsmaeker Stijn Glorie Fedor Zhimulev Marc Jolivet Martin Danisík Mikhail M.Buslov Johan De Grave | 2018 | Geoscience Frontiers2018，9，5： | 4 |
| 5 | 脊髓损伤后残存自主神经功能载录国际标准显示文摘近年来,脊髓损伤神经学分类园际标准(International Stand- ards for the Neurological Classification of Spinal Cord Injury, ISNCSCI)被用来记载脊髓损伤后运动和感觉功能的损害,目前该标准已是第六版。1992年第一份国际认可的标准出版时,曾进行了较大的修订,修订内容包括完全性损伤与不完全性损伤的定义, | MS Alexander AB Jackson W Donovan DE Graves SL Elliott A Krassioukov AW Sheel I Estoresl B Green A Gousse NL Braekett D Cardenas M Kennelly A-K Karlason F Biering-Sorensen K Krogh T Linsenmeyer R Marino J Ditunno CJ Mathias I Perkash G Creasey G Schilero J Wecht B Schurch V Dietz J Sonksen S Stiens D Bodner LA Wuermser J-J Wyndaele 周谋望 刘楠 S Charlifue | 2010 | 中华物理医学与康复杂志2010，32，4： | 2 |
| 6 | Problem_based learning:future challenges for educational practice and research显示文摘 | De Grave W Wolfhagen IH | 2005 | Med Educ2005，39，7： | 1 |
| 7 | Sediment quality guidelines and assessment: over and research needs 显示文摘 | McCauley D J De Grave G M Linton T K | 2000 | Environmental Sciences and Policy2000，3，： | 1 |
| 8 | Problem-based learning: future challenges for educational practice and research 显示文摘 | Dolmans DH De Grave W Wolfhagen IH | 2005 | Med Educ2005，39，7： | 1 |
| 9 | Problem-based learning:future challenges for educational practice and research显示文摘 | Diana HJM Dolmans Willem De Grave Ineke HAP Wolfhagen | 2005 | Medical Education2005，，39： | 1 |
| 10 | Problem-b ase dl eaming:fu turec halengesf ore ducationalp racticeand research显示文摘 | Dolmans DH De Grave W Wolfhagen IH | | 0，，07： | 1 |
| 11 | Problem-based learning:future challenges for educationalpractice and research显示文摘 | Dolmans DH De Grave W Wolfhagen IH | 2005 | Medical Education2005，39，7： | 1 |
| 12 | Problem- based learning: future challenges for educational practice and research显示文摘 | Dolmans Dtt De Grave W Wolfhagen IH | 2005 | Med Educ2005，39，7： | 1 |
| 13 | Sediment quality guidelines and assessment:over and research needs显示文摘 | McCauley D J De Grave G M Linton T K | 2000 | Environmental Sciences and Policy2000，3，： | 1 |
| 14 | Problem-based learning:future challenges for educational practice and research显示文摘 | Dolmans DH De Grave W Wolfhagen IH | 2005 | Med Educ2005，39，7： | 1 |
| 15 | Problem-based learning:future challenges for educational practice and research显示文摘 | Dolmans DH De Grave W Wolfhagen IH | 2005 | Med Educ2005，39，7： | 1 |
| 16 | ProblemBased Learning:Future Challenges for Educational Practice and Research显示文摘 | Dolmans DH De Grave W Wolfhagen IH | 2005 | Med Educ2005，39，7： | 1 |
| 17 | Problem- based learning:future challenges for educational practice and research显示文摘 | Dolmans DH De Grave W Wolfhagen IH | 2005 | Med Educ2005，39，7： | 1 |
| 18 | Problem - based learning:future challenges for educational practice and research 显示文摘 | Dolmans DH De Grave W Wolfhagen IH | 2005 | Med Educ2005，39，7： | 1 |
| 19 | Problem-based learning: Future challenges for educational prac- tiee and research 显示文摘 | Dolmaus DHJM De Grave W Wolfhagen IHAP Van der Vleuten CPM | 2005 | Medical Education2005，39，： | 1 |
| 20 | Quantifying lower limb joint position sense using a robotic exoskele- ton: a pilot study显示文摘 | Domingo A Marriott E de Grave RB | 2011 | IEEE Int Conf Rehabil Robot2011，，59： | 1 |
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