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| 1 | 昆仑山深部结构与造山机制显示文摘本文根据INDEPTH-Ⅳ剖面所做的地质、地球物理探测所取得的资料,进行综合研究,提出了一个新的昆仑山造山模式,论述了:(1)在早二叠世松潘—甘孜洋向昆仑—柴达木地块下俯冲使地块南缘形成陆缘弧和弧后拉张区,使昆仑—柴达木地块在持续碰撞挤压过程中,分别形成了造山带与古近—新近纪盆地的不同构造演化特征;(2)昆仑地段老结晶基底在地块对挤中不断向上抬升成山,同时又受到强烈剥蚀,使老结晶基底及深成岩呈现在地表;南昆仑地块则沿昆仑地块中央断裂向北逆冲到北昆仑地块之上,断裂深10km;昆仑地块没有发生向北逆冲推覆到柴达木地块上;(3)昆仑地块地壳增厚主要发生在中地壳(6.2~6.6 km/s),是中基性岩石层的增厚;(4)柴达木盆地作为昆仑弧弧后拉张地带,随昆仑造山隆升而下沉,新生界陆相沉积达12~14km厚,由“沉积”与“挤入”两个作用造成了地壳增厚;结晶基底发生断陷形成新裂谷,裂谷宽度约12km,深度约4km,导电带显示裂谷通过断裂与深部发生热流体联系;(5)再次确定了,柴达木盆地莫霍界面深52 km,昆仑山的莫霍界面深65~70 km,莫霍界面台阶位于格尔木附近(185km距离处);(6)松潘—甘孜地体复理石层厚度为10~14 km,其下面的6.2~6.3 km/s均匀速度层(同时有高导电性显示)是本地块所特有,推测为残留洋壳的堆积,约15km厚;浅层通过古近—新近系风火山推覆系增厚,另在中地壳部位挤入了15km厚岩层;(7)否定了亚洲岩石圈地幔向柴达木地块地幔岩石圈之下俯冲的模式,提出印度大陆地幔岩石圈从高喜马拉雅下拆离成两层,并沿高原地壳底部向北伸展,直到中祁连山之下,成为高原南北对挤过程中岩石圈地幔长度调节的新方式. | 赵文津 吴珍汉 史大年 薛光琪 宿和平 Karplus M S Mechie J 宋洋 杨宏伟 刘志伟 | 2014 | 中国地质2014，41，1： | 15 |
| 2 | 走向成熟的中国植物生物学研究显示文摘近年来,中国大陆植物生物学的研究取得了举世瞩目的进展,这直接体现在过去15年间一些主要植物专业杂志和综合性学术刊物上发表论文的数量。中国植物学研究之所以能够取得如此辉煌的成就,一方面是得益于早期中国植物学研究所奠定的基础,另一方面则应归功于中国改革开放政策的实施。通过描述中国的一些代表性研究机构的发展历程,以及总结它们在水稻和拟南芥两大植物研究领域中所取得的突破,我们清晰地看到了中国植物学研究的光辉前景,但是挑战依然存在。 | 陈浩东 Karplus J.Valerie 马红 邓兴旺 李继刚 | 2007 | 中国农业科技导报2007，9，4： | 6 |
| 3 | The thickness and structural characteristics of the crust across Tibetan plateau from active-sources seismic profiles显示文摘The Tibetan plateau as one of the youngest orogen on the Earth was considered as the result of continent-continent collision between the Eurasian and Indian plates.The thickness and structure of the crust beneath Tibetan plateau is essential to understand deformation behavior of the plateau.Active-source seismic profiling is most available geo-physical method for imaging the structure of the continental crust.The results from more than 25 active-sources seismic profiles carried out in the past twenty years were reviewed in this article.A preliminary cross crustal pattern of the Tibetan Pla-teau was presented and discussed.The Moho discontinuity buries at the range of 60-80 km on average and have steep ramps located roughly beneath the sutures that are compatible with the successive stacking/accretion of the former Cenozoic blocks northeastward.The deepest Moho(near 80 km) appears closely near IYS and the crustal scale thrust system beneath southern margin of Tibetan plateau suggests strong dependence on collision and non-distributed deformation there.However,the ~20 km order of Moho offsets hardly reappears in the inline section across northern Tibetan plateau.Without a universally accepted,convincing dynamic explanation model accommodated the all of the facts seen in controlled seismic sections,but vertical thickening and northeastern shorten of the crust is quite evident and interpretable to a certain extent as the result of continent-continent collision.Simultaneously,weak geophysical signature of the BNS suggests that convergence has been accommodated perhaps partially through pure-shear thickening accompanied by removal of lower crustal material by lateral escape.Recent years the result of Moho with ~7 km offset and long extend in south-dip angle beneath the east Kunlun oro-gen and a grand thrust fault at the northern margin of Qilian orogen has attract more attention to action from the northern blocks.The broad lower-velocity area in the upper-middle crust of the Lhasa block was once considered as resulted from partially melted rocks.However the low normal vP/vS ratio and the Moho stepwise rise fail to support significant partial melting in the middle-lower crust of the central-northern Tibetan plateau.Furthermore,the lower-velocity of crust occasionally disappears,and/or local thinned exhibits their non-stationary spatial distribution. | Qiusheng Li Rui Gao Zhanwu Lu Ye Guan Jisheng Zhang Pengwu Li Haiyan Wang Rizheng He Marianne Karplus | 2009 | Earthquake Science2009，22，1： | 5 |
| 4 | Prediction of chain flexibility in protein显示文摘 | KARPLUS P A | 1985 | Immunology1985，72，2： | 1 |
| 5 | Sequence comparisons using multiple sequences detect three times as many remote homo-logues as pairwise methods显示文摘 | Karplus K Barrett C | 1998 | J Mol Biol1998，284，4： | 1 |
| 6 | Combining local-structure, fold-recognition, and new-fold methods for protein structure prediction显示文摘 | Karplus K Karchin R Draper J | 2003 | Proteins2003，53，： | 1 |
| 7 | How enzymes work:analysis by modern rate theory and computer simulations显示文摘 | Garcia-Viloca M Gao J Karplus M | 2004 | Science2004，303，： | 1 |
| 8 | Molecular dynamics simulations in biology 显示文摘 | Karplus M Petsko G A | 1990 | Nature1990，347，6294： | 1 |
| 9 | Predicting protein structure using only sequence information 显示文摘 | Karplus K Barrett C DiekhansM | 1999 | proteins: Structure Function and Bioinformatics1999，3，： | 1 |
| 10 | Neural networks for secondary structure and structural class prediction 显示文摘 | Chandonia J M Karplus M | 1995 | Protein Science1995，，4： | 1 |
| 11 | Predicting protein structure using Hidden Markov Models 显示文摘 | Karplus K Sj lander K Barrett C | 1997 | Proteins : Structure Function and Genetics1997，1，： | 1 |
| 12 | Prediction of chain flexibility in proteins显示文摘 | KARPLUS P SCHULZ G | 1985 | Naturwissenschaften1985，72，4： | 1 |
| 13 | In - vivo fish sorting by computer vision 显示文摘 | ZION B SHKLYAR A KARPLUS I | 2000 | Agricultural Engineering2000，22，3： | 1 |
| 14 | Prediction of chain flexibility in proteinsa tool for the selection of peptide antigens显示文摘 | Karplus PA Schulz GE | | 0，，： | 1 |
| 15 | First-order disorder-to-order transition in an isolated homopolymer model 显示文摘 | Zhou Y Q Hall C K Karplus M | 1996 | Physical Review Letters1996，77，13： | 1 |
| 16 | Kinetics of protein folding显示文摘 | Sali A Shakhnovich E Karplus M | 1994 | Journal of Molecular Biology1994，235，5： | 1 |
| 17 | Folding of a model three-helix bundle protein: A thermodynamic and kinetic analysis 显示文摘 | Zhou Y Q Karplus M | 1999 | Journal of Molecular Biology1999，293，4： | 1 |
| 18 | Prediction of chain flexibility in proteins显示文摘 | Karplus P A Schultz G E | 1985 | Immunology1985，72，2： | 1 |
| 19 | Vicinal proton coupling in nuclear magnetic resonance 显示文摘 | KARPLUS M | 1963 | J Am Chem Soc1963，85，18： | 1 |
| 20 | Identification of prokaryotic small proteins using a comparative genomic approach显示文摘 | Samayoa J Yildiz F H Karplus K | 2011 | Bioinformaties2011，27，13： | 1 |
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