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| 1 | Insights into the Tectonic Fractures in the Yanchang Formation Interbedded Sandstone-Mudstone of the Ordos Basin Based on Core Data and Geomechanical Models显示文摘The distribution and intensity of tectonic fractures within geologic units are important to hydrocarbon exploration and development. Taken the Upper Triassic Yanchang Formation interbedded sandstone-mudstone in the Ordos Basin as an example, this study used the finite element method(FEM) based on geomechanical models to study the development of tectonic fractures. The results show that the sandstones tend to generate tectonic fractures more easily than mudstones with the same layer thickness, and the highest degree of tectonic fractures will be developed when the sandstone-mudstone thickness ratio is about 5.0. A possible explanation is proposed for the tectonic fracture development based on two important factors of rock brittleness and mechanical layer thickness. Generally, larger rock brittleness and thinner layer thickness will generate more tectonic fractures. In interbedded sandstone-mudstone formations, the rock brittleness increases with the increasing mechanical layer thickness, hence, these two factors will achieve a balance for the development of tectonic fractures when the sandstone-mudstone thickness ratio reaches a specific value, and the development degree of tectonic fractures is the highest at this value. | JU Wei SUN Weifeng HOU Guiting | 2015 | Acta Geologica Sinica(English Edition)2015，89，6： | 16 |
| 2 | Mesozoic-Cenozoic extension of the Bohai Sea: contribution to the destruction of North China Craton显示文摘Bohai 海是位于东方诺思中国 Craton (NCC ) 的盆山脉系统的一个迟了的中生代新生代特征。岩石圈变瘦的迟了的中生代表明 NCC 的早破坏。破坏的发作由于 craton 的厚岩石圈的分层,在 Tanlu 差错地区以内向西在在军队飞机安排由趋势 NW grabens,并且由趋势 NNE grabens 代表了到 Tanlu 差错。迟了的中生代趋势 NW grabens 被与新生代趋势 NE 拉开盆有关的结构在东方 NCC 与很厚的中生代新生代沉积套印。生长差错和延期因素的 C 频率图([贝它]) 四,越过盆的节建议延期从边缘移居了到 Bohai 海的中心,并且为 Bohai 海的中生代和新生代延期因素比边缘的高。这些证据建议最大的延期发生在 Bohai 海的中心,它与在海的中心被发现的最薄的外壳一致。延期比率和 Bohai 海的构造进化建议它是为 NCC 的破坏的关键区域,由地形学证实了。然而, NCC 与与东北亚洲的构造政体有关的迟了的阶段经历了破坏的二个阶段[出版摘要] | Guiting HOU K. R. HARI | 2014 | Frontiers of Earth Science2014，8，2： | 14 |
| 3 | The late Paleoproterozoic extension event:aulacogens and dyke Swarms in the North China craton显示文摘在北方中国 Craton (NCC ) 的延期结构和构造牵连基于 mafic 塘群和地球年代学在这篇论文被讨论,与 aulacogens 的地球年代学结合。迟了的 Paleoproterozoic 时间是在 NCC 的前寒武纪的进化的重要拐弯处点。延期系统(例如 aulacogens 和塘群) 在 NCC 是普遍的,它与类似于现代的板的僵硬特征标记 NCC 的碳化。当模特儿的 paleostress 地建议塘聚集, aulacogens 是标记超级大陆,不是 synorogenic 的开始的 arogenic 扩展和 postorogenic 扩展。在 NCC 的 mafic 塘群主要从 1.83 ~ 1.77 Ga 。NCC 的延期是很有限的易碎的扩展,平均延期比率仅仅是 0.35% 由 mafic 塘群延期计算给,大多数在 NCC 的扩展被 aulacogens 因此贡献。mafic 塘群在起源与 aulacogens 被联系。 | HOU Guiting LI Jianghai LIU Yulin QIAN Xianglin | 2006 | Progress in Natural Science:Materials International2006，16，2： | 13 |
| 4 | Fractal Simulation and Classification of Folds显示文摘The method of fractal simulation and classification of folds is firstly studied here to describe various types of complex fold patterns in quantitative analysis. Based on the characteristics of natural folds with a fractal pattern, the fold patterns are simulated to describe various types of folds quantitatively by means of fractal interpolation. The major factors affecting the fold pattern are elucidated in fractal simulation of folds, i.e. positions of interpolation points (x, y) and the disturbance coefficient d of folds (-1<d<1). The bigger the value d for a fold simulation is, the more complex or disturbed the folds are and the better developed the relative secondary folds are. If d>0, folds are up-convex. IF d<0, they are down-convex. |d|=0, |d|=0.25 and |d|=0.5 represent three conspicuous turning states. If |D|=0, the points will be joined by a straight line. If |d|=0.25, the points will be joined smoothly. If |d|>0.25, there will be complex secondary folds between the points. If |d| >0.5, | HOU Guiting | 1998 | Acta Geologica Sinica(English Edition)1998，72，2： | 7 |
| 5 | Possibility of the Application of the Ultra-long Electromagnetic Wave Remote Sensor to Marine Geological Exploration显示文摘The ultra-long electromagnetic wave remote sensing technique developed by Peking University is one of new future techniques, which can detect the submarine geological information from the depth of 20 to 10000 m below the surface by receiving natural ultra-long electromagnetic waves (n Hz to n 100 Hz). The new remote sensor is composed of three parts: a main instrument with a portable computer, an antenna with an amplifier and an external power.The new remote sensing technique is characterized by good stability and reproducibility at the same spot but at different times and high sensitivity and high signal-to-noise ratio, and can reveal geological and lithologic boundaries as well as strata and related mineral sources. Two years of marine geological experiments on this technique have indicated that it can solve many problems in marine geological exploration, e.g. the burial depths of sea-floor mud, Quaternary sediments and submarine structures. This technique can be applied to detecting the sea bed | HOU Guiting QIAN Xianglin WANG Shuyuan SUN Jing | 2000 | Acta Geologica Sinica(English Edition)2000，74，2： | 6 |
| 6 | Mechanism for three types of mafic dyke swarms显示文摘这研究建议三个模型解释 mafic 塘群的三种主要类型的机制。而小放射塘群在一座 Pluto 或暴烈的大厦附近由于压力构造形成,平行的塘群响应地区性的压力域形成,例如在北方中国 Craton 的 mafic 塘群,例如在西班牙的山峰的塘群,美国。散发塘群的第三种类型是象 Mackenzie 塘群那样的巨大的扇形的塘群。在 magmatism 以前形成了的破裂可以在支配塘群几何学起一个重要作用。在大多数盒子中,尽管岩浆注射能在塘尖端由繁殖增加破裂尺寸,先存在的破裂被构造压力并且不由岩浆注射导致。 | Guiting Hou | 2012 | Geoscience Frontiers2012，3，2： | 6 |
| 7 | Wind vector retrieval using dual polarization imagery of ASAR显示文摘A new algorithm for retrieving wind vector using dual polarization imagery of advanced synthetic aperture radar (ASAR) is developed and tested. Based on the combination of co-polarization and cross-polarization, this new algorithm effectively eliminates the 180° ambiguity which occurs when using single imagery of the ASAR to retrieve wind vector. This algorithm also solves the problem that the retrieval results will break down on very small spatial scales. The results retrieved from dual polarization imagery of ASAR show that the wind speed and direction are in agreement with the data from Quikscat and buoy measurements. The root mean square errors of wind direction and speed between the retrieved results and data from Quikscat are 2.21° and 0.53 m/s, respectively. Comparisons between the new method and the traditional method show that the new methods fit the buoy data and Quikscat data a little better than the traditional method in this image. | SONG Guiting HOU Yijun QI Peng | 2006 | Progress in Natural Science:Materials International2006，16，11： | 5 |
| 8 | End Late Paleozoic tectonic stress field in the southern edge of Junggar Basin显示文摘这份报纸论述在由解释压力反应的 Junggar 盆的南部的边的晚古生代的构造压力地组织的结束(女同性恋,褶层,有岩石光滑面的差错并且结合关节) 。最大的主要压力轴的方向被解释是 NWSE (大约 325 牥污 ? 整浲吗? | Wei Ju Guiting Hou Le Li Fangfeng Xiao | 2012 | Geoscience Frontiers2012，3，5： | 5 |
| 9 | Late Permian to Triassic intraplate orogeny of the southern Tianshan and adjacent regions, NW China显示文摘The South Tianshan Orogen and adjacent regions of Central Asia are located in the southwestern part of the Central Asian Orogenic Belt.The formation of South Tianshan Orogen was a diachronous,scissors-like process,which took place during the Palaeozoic,and its western segment was accepted as a site of the fnal collision between the Tarim Craton and the North Asian continent,which occurred in the late Palaeozoic.However,the post-collisional tectonic evolution of the South Tianshan Orogen and adjacent regions remains debatable.Based on previous studies and recent geochronogical data,we suggest that the fnal collision between the Tarim Craton and the North Asian continent occurred during the late Carboniferous.Therefore,the Permian was a period of intracontinental environment in the southern Tianshan and adjacent regions.We propose that an earlier,small-scale intraplate orogenic stage occurred in late Permian to Triassic time,which was the frst intraplate process in the South Tianshan Orogen and adjacent regions.The later largescale and well-known Neogene to Quaternary intraplate orogeny was induced by the collision between the India subcontinent and the Eurasian plate.The paper presents a new evolutionary model for the South Tianshan Orogen and adjacent regions,which includes seven stages:(I)late Ordovicianeearly Silurian opening of the South Tianshan Ocean;(II)middle Silurianemiddle Devonian subduction of the South Tianshan Ocean beneath an active margin of the North Asian continent;(III)late Devonianelate Carboniferous closure of the South Tianshan Ocean and collision between the Kazakhstan-Yili and Tarim continental blocks;(IV)early Permian post-collisional magmatism and rifting;(V)late PermianeTriassic the frst intraplate orogeny;(VI)JurassicePalaeogene tectonic stagnation and(VII)NeoceneeQuaternary intraplate orogeny. | Wei Ju Guiting Hou | 2014 | Geoscience Frontiers2014，5，1： | 2 |
| 10 | Alkali feldspar syenites with shoshonitic affinities from Chhotaudepur area: Implication for mantle metasomatism in the Deccan large igneous province显示文摘Two petrologically distinct alkali feldspar syenite bodies(AFS-1 and AFS-2) from Chhotaudepur area,Deccan Large Igneous Province are reported in the present work. AFS-1 is characterized by hypidiomorphic texture and consists of feldspar(Or55Ab43to Or25Ab71), ferro-pargasite/ferro-pargasite hornblende, hastingsite, pyroxene(Wo47, En5, Fs46), magnetite and biotite. AFS-2 exhibits panidiomorphic texture with euhedral pyroxene(Wo47-50, En22-39, Fs12-31) set in a groundmass matrix of alkali feldspar(Or99Ab0.77to Or1.33Ab98), titanite and magnetite. In comparison to AFS-1, higher elemental concentrations of Ba, Sr andPREE are observed in AFS-2. The average peralkaline index of the alkali feldspar syenites is w1 indicating their alkaline nature. Variation discrimination diagrams involving major and trace elements and their ratios demonstrate that these alkali feldspar syenites have a shoshonite affinity but emplaced in a within-plate and rifting environment. No evidence of crustal contamination is perceptible in the multi-element primitive mantle normalized diagram as well as in terms of trace elemental ratios. The enrichment of incompatible elements in the alkali feldspar syenites suggests the involvement of mantle metasomatism in their genesis. | K.R.Hari N.V.Chalapathi Rao Vikas Swarnkar Guiting Hou | 2014 | Geoscience Frontiers2014，5，2： | 1 |
| 11 | Late Paleoproterozoic extension and a paleostress field reconstruction of the North China Craton显示文摘 | Guiting Hou Chuancheng Wang Jianghai Li Xianglin Qian | 2006 | Tectonophysics2006，，1： | 1 |
| 12 | Late Paleoproterozoic extension and a paleo - stress field reconstruc- tion of the North China Craton 显示文摘 | Guiting Hou Chuancheng Wang Jianghai Li Xianglin Qian | 2006 | Tectonophysics2006，422，14： | 1 |
| 13 | Rheological Properties of Fractal Deformation in Multilayer Folds显示文摘褶层的分数维的尺寸与层厚度和粘性有关多层。这篇论文讨论厚度,粘性,和各向异性的度怎么影响分数维图形的逻辑变丑在 multilayers 合拢的变阻器。multilayers 的层,他们的厚度,粘性,和各向异性的度的数字合作影响变阻器逻辑变丑合拢逻辑因素,它没被一个单个变阻器控制。multilayers 的更大的各向异性的度是有利的开发更复杂、不调和的分数维的褶层。 | HOU Guiting | 2009 | Acta Geologica Sinica(English Edition)2009，83，3： | 1 |
| 14 | Mechanics of Mafic Dyke Swarms and Breakup of Supercontinent显示文摘Dyke swarms can be divided into three types:parallel dyke swarms,radiating dyke swarms and fan-shape dyke swarm,for which the mechanisms of formation are different(Fig.1).Parallel dyke swarms form in | HOU Guiting | 2016 | Acta Geologica Sinica(English Edition)2016，90，S1： | 1 |
| 15 | Dyke Emplacement in the Narmada Rift Zone and Implications for the Evolution of Deccan Traps显示文摘Dykes are primarily extensional fractures that form perpendicular to the minimum principal compressive stress,which have been extensively studied in the world during the past decades for various reasons including | JU Wei HOU Guiting K.R.HARI | 2016 | Acta Geologica Sinica(English Edition)2016，90，S1： | 0 |
| 16 | Cretaceous Stress Fields Evolution and Its Geodynamic Implications in Jiaolai Basin, Northern China显示文摘The Tan-Lu fault zone(TLFZ)along the East China continental margin experienced sinistral movement at the beginning of Early Cretaceous(ca.145)due to fast oblique subduction of the Izanagi Plate in the Pacific Ocean.It | LI Jie HOU Guiting | 2016 | Acta Geologica Sinica(English Edition)2016，90，S1： | 0 |
| 17 | Mechanism of the Formation of the East African Rift System显示文摘The East African Rift System(EARS)is located in East Africa,separating into two main branches,the eastern branch and the western branch.It is considered as an intracontinental ridge system,which meets the Red Sea | MIN Ge HOU Guiting | 2016 | Acta Geologica Sinica(English Edition)2016，90，S1： | 0 |
| 18 | Mechanism of Zhongtiao Aulacogen Related to Breakup of Columbia Supercontinent显示文摘The mechanism of the breakup of supercontinent is a scientific frontier in the field of supercontinent study.The rifting and breakup of supercontinent has long been considered to be related to mantle plume.Paleo- | SUN Shuai HOU Guiting | 2016 | Acta Geologica Sinica(English Edition)2016，90，S1： | 0 |
| 19 | Dynamic Controls on the Formation of Mantle Plume Beneath the South China Sea Region显示文摘The South China Sea(SCS)has attracted intensive structural and geophysical research over the past decades,with a focus on its extensional history and relevant dynamic tectonic models.Seismic tomographic images | YU Xuan HOU Guiting | 2016 | Acta Geologica Sinica(English Edition)2016，90，S1： | 0 |
| 20 | Evolution of the Nanhua-Sinian Rifts in the Tarim Block显示文摘The Tarim block,located in northwestern China,is one of the largest blocks in China.Precambrian rifts in the Tarim block control the evolution of Paleozoic rifts.On the basis of previous research by other authors,and | ZHENG Chunfang HOU Guiting GUAN Shuwei | 2016 | Acta Geologica Sinica(English Edition)2016，90，S1： | 0 |
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