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| 1 | Central Asian aridification during the late Eocene to early Miocene inferred from preliminary study of shallow marine-eolian sedimentary rocks from northeastern Tajik Basin显示文摘The tempo-spatial development of the Cenozoic Asian aridification across the Eocene-Oligocene and its controlling factors are important scientific topics in Earth Sciences, which are pertinent to regional and global tectonic and climatic events. However, sedimentary rocks preserving the record of aridification during this time from central Asia(ACA) are rare. Here we present a preliminary analysis of sedimentary facies of the lower Paleogene in the northeastern Tajik Basin, which reveals that: the lower part of the studied section is dominated by shallow marine deposits of the Paratethys, the middle part is typical of alternations of eolian dune and fluvial deposits, the upper part is represented by eolian loess-sandy loess(L&SL) like facies, and the top exhibits alternations of fluvial-lacustrine and loess like facies. Based on a chronological framework derived from preliminary magnetostratigraphy, published U-Pb dating of a volcanic ash, and regional litho-stratigraphic correlations, we determine that eolian and L&SL facies accumulated in the northeastern Tajik Basin during the Late Eocene and through most of the Oligocene. These sedimentary units indicate that semi-arid to arid environments of ACA had developed at least since the late Eocene. This initial aridification is closely linked to the westward retreat of the Paratethys that was likely driven by a combination of tectonic activity and sea level changes. | WANG Xin Brian KRAATZ Jin MENG Barbara CARRAPA Peter DECELLES Mark CLEMENTZ Sherzod ABDULOV CHEN FaHu | 2016 | Science China Earth Sciences2016，59，6： | 9 |
| 2 | 塔吉克盆地东北缘海相-风成沉积序列与中亚晚始新世-早中新世干旱化的初步研究显示文摘新生代亚洲内陆干旱化的时空演化历史及其驱动机制,是国际古环境研究的热点和重点,然而至今缺少直接来自中国境外干旱区的新生代干旱化记录.对塔吉克盆地东北缘代表性剖面的沉积相分析结果表明,该地区早新生界地层底部以副特提斯海沉积序列为主,中部为厚层风成砂与河流砂交互沉积,上部以风成黄土、砂黄土状堆积为主,顶部为河湖相沉积和风成黄土状堆积交互沉积.根据已发表的火山灰U-Pb年代、初步的古地磁年代框架及区域地层划分证据,风成砂和黄土、砂黄土状堆积物形成于晚始新世和渐新世,表明中亚的干旱环境可能从始新世晚期已经开始,其形成和发展与构造活动驱动的晚始新世副特提斯海退缩密切相关. | 王鑫 Brian KRAATZ Jin MENG Barbara CARRAPA Peter DECELLES Mark CLEMENTZ Sherzod ABDULOV 陈发虎 | 2016 | 中国科学:地球科学2016，46，5： | 5 |
| 3 | Restricted Boltzmann machine: Recent advances and mean-field theory显示文摘This review deals with restricted Boltzmann machine(RBM) under the light of statistical physics.The RBM is a classical family of machine learning(ML) models which played a central role in the development of deep learning.Viewing it as a spin glass model and exhibiting various links with other models of statistical physics,we gather recent results dealing with mean-field theory in this context.First the functioning of the RBM can be analyzed via the phase diagrams obtained for various statistical ensembles of RBM,leading in particular to identify a compositional phase where a small number of features or modes are combined to form complex patterns.Then we discuss recent works either able to devise mean-field based learning algorithms;either able to reproduce generic aspects of the learning process from some ensemble dynamics equations or/and from linear stability arguments. | Aurélien Decelle Cyril Furtlehner | 2021 | Chinese Physics B2021，30，4： | 2 |
| 4 | Foreland basin systems显示文摘 | Decelles P G Giles K A | 1996 | Basin Research1996，8，2： | 1 |
| 5 | Inference and phase transitions in the detection of modules in sparse networks显示文摘 | Decelle A Krzakala F Moore C | 2011 | Physical Review Letters2011，107，06： | 1 |
| 6 | Initiation of the Himalayan orogen as an early Paleozoic thin-skinned thrust belt 显示文摘 | Gehrels G E Decelles P G Martin A | 2003 | GSA Today2003，，9： | 1 |
| 7 | Late Cretaceous-Paleoeene synorogenic sedimentation and kinematic history of the Sevier thrust belt, Northeast Utah and Southwest Wyoming显示文摘 | DeCelles P G | 1994 | Geological Society of American Bulletin1994，106，： | 1 |
| 8 | Detrital zircon geochronology of pre-Tertiary strata in the Tibetan-Himalayan orogen显示文摘 | GEHRELS G KAPP P DECELLES P | 2011 | Tectonics2011，30，： | 1 |
| 9 | Detrital geochronology and geochemistry of Cretaceous-Early Miocene strata of Nepal:implications for timing and diachroneity of initial Himalayan orogenesis显示文摘 | DECELLES P G GEHRELS G E NAJMAN Y | 2004 | Earth and Planetary Science Letters2004，227，34： | 1 |
| 10 | Forland basin systems 显示文摘 | Decelles G & Gilest | 1996 | Basin Research1996，8，： | 1 |
| 11 | Geological Recordsof the Lhasa-Qiangtang and Indo-Asian Collisions in the Ni-ma Area of Central Tibet显示文摘 | Kapp P Decelles P G Gehrels G E | 2007 | Geological Society of AmericaBulletin2007，119，78： | 1 |
| 12 | Multiple micro- organisms in chalkbrood mummies: evidence and implications 显示文摘 | Johnson RN Zaman MT Decelle MM | 2005 | Journal Apiculture Research2005，44，1： | 1 |
| 13 | Foreland basin systems显示文摘 | DeCelles P G Giles K A | 1996 | Basin Research1996，8，： | 1 |
| 14 | Foreland basin systems basin research 显示文摘 | Decelles P G Giles K A | 1996 | Blackwell Science Ltd Basin Research1996，8，： | 1 |
| 15 | Geologic control of Sr and major element chemistry in Himalayan Rivers,Nepal显示文摘 | English N B Quade J Decelles P G | 2000 | Geochimica et Cosmochimica Acta2000，64，13： | 1 |
| 16 | Foreland basin system 显示文摘 | DeCelles P G Giles K A | 1996 | Basin Research1996，8，： | 1 |
| 17 | Oligocene-rmocene Kailas Basin, Southwestern Tibet Record of Postcollisional Upper-plate Extension in the Indus-yarlung Suture Zone显示文摘 | Decelles P G Kapp P Quade J | 2011 | Geological Society of America Bulletin2011，123，7： | 1 |
| 18 | The late Neogene ^87Sr/ ^86Sr record of lowland Himalayan rivers显示文摘 | Quade J Roe L Decelles P G | 1997 | Science1997，276，： | 1 |
| 19 | Tectonic implications of U-Pb zircon ages of the Himalayan Orogenic Belt in Nepal显示文摘 | DeCelles P G Gehrels G E Quade J | 2000 | Science2000，288，5456： | 1 |
| 20 | Gangdese retroarc thrust belt and foreland basin deposits in the Damxung area, southern Tibet显示文摘 | Alex Pullen Paul Kapp George E. Gehrels Peter G. DeCelles Edwin H. Brown J. Matthew Fabijanic Lin Ding | 2008 | Journal of Asian Earth Sciences2008，，5： | 1 |
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