滇西北新生代逆冲推覆构造

滇西北地区新生代逆冲推覆构造较为发育，从西到东可分出走向NS、相互平行的4带：澜沧江带，云岭带，石钟山带和剑川-洱源带。其中，澜沧江带与云岭带组成对冲格局，云岭带又与石钟山带组成反冲格局，石钟山带与剑川-洱源带又组成对冲格局。参与逆冲推覆的地层主要是中生代三叠系、侏罗系、白垩系及新生代云龙组、宝相寺组，推覆体由石炭系、二叠系、上三叠统岩石组成。逆冲推覆时间为喜马拉雅期。     

晚太古代Sanukite（赞岐岩）与地球早期演化

Shirey and Hanson(1984)将某些太古代的高镁闪长岩套称为sanukite(赞岐岩),类似于日本中新世(11～15Ma)Setouchi火山岩带的高镁安山岩。Sanukitoids由闪长岩-二长闪长岩-花岗闪长岩组成,不同于TTC岩套(奥长花岗岩-英云闪长岩-花岗闪长岩)。Sanukitoids具有下列地球化学特征:富Mg,Mg~#>0.60,Ni和Cr>100μg/g,Sr和Ba>500μg/g,LREE富集(大于球粒陨石100倍),无Eu异常。高镁安山岩在太古代很少见,而其相应的侵入岩高镁闪长岩或sanukitoids,虽然数量也很少,但却是各地晚太古代地体中随处可见的。Sanukitoids的原始岩浆是交代的地幔楔部分熔融形成的,随后可能经历了广泛的分离结晶作用。TTC和sanukitoids岩套可以相伴产出,二者均与板片熔融有关,TTG与其直接有关,sanukitoids可能与其间接有关。全球Sanukitoids主要集中在晚太古代时期,可能暗示板块的消减作用在～3.0Ga以后才起了重要的作用。     

与时俱进,发展中国大地构造学

论述了黄汲清经典著作《中国主要地质构造单位》的深远影响。它是中国大地构造研究的奠基之作和经典著作 ,其基本内容和主要论点已为实践所证实 ,并为国内外地质界所认同。这部著作不仅全面系统地总结了过去 ,而且对一些重大地质问题进行了科学预测 ,为后人指出了研究的方向。它是一部你什么时候读都有味道 ,都会受到新的启发的著作。黄汲清的学术思想是民主的、开放的 ,与时俱进的。在《中国主要地质构造单位》中 ,他运用阿尔冈活动论的思想 ,阐述了中国大地构造的动力演化过程。之后 ,他又吸收了裴伟深断裂的思想 ,深入研究了中国的深断裂。 2 0世纪 70年代 ,他指导他的学生将多旋回思想与板块构造结合 ,在中国大地构造图上首次详细标绘了中国境内的板块缝合带 ,从全球动力学角度 ,将他 1 94 5年提出的亚洲三种构造型式发展为古亚洲、特提斯和滨太平洋三大构造域。黄汲清的研究始终是从东亚地质的实际情况出发 ,他曾多次指出 :中国是全球构造研究中的一块宝地 ,中国人应该为世界地质科学的发展做出贡献     

内蒙古大青山地区构造特征与成矿关系

内蒙古大青山地区的临河-集宁断裂带是华北板块北缘的一条重要断裂带,它主要由韧性剪切带、韧脆性剪切带和推覆构造等构成.推覆构造自南向北可分为叠瓦逆冲推覆构造带、紧闭褶皱一逆冲断层变形带、宽缓褶皱-断层转折褶皱带、滑脱褶皱-断层传播褶皱带等4个变形带.断裂带从韧性到脆性表示了其出露深度不同,并有由南到北活动强度逐渐减弱的趋势.该区主要分布有以金为主的多金属矿床和以煤、大理岩为主的非金属矿床.区内金多金属矿床多与韧性剪切带有关,断裂构造为金属矿床的形成提供了空间,也是成矿物质的通道.研究指出了该地区的找矿前景与方向.     

中国东部中新生代构造格局和岩浆岩带的形成与演化

在研究印支期秦岭-大别-苏鲁造山带的形成与地幔差速环流的基础上，系统综合了中国东部中新生代的基底构造对断裂构造的控制，深层构造对隆凹与断陷盆地的制约，伸展构造在陆内及陆缘外的表现，岩浆岩带的时空分布及展布特点等规律，依据中国东部中新生代构造格局与岩浆岩带在时空分布上的宽阔性、方向性、迁移性、分带性，特别是深层构造对浅层断裂构造、伸展构造的制约，以及岩浆岩带、隆起与盆地等自西向东迁移特点，提出其形成机制可能与强大地幔东向差速环流有关。     

辽西医巫闾山地区中生代两期韧性变形的研究

医巫闾山地区的韧性剪切构造是中生代两期韧性变形作用的产物。早期韧性变形中a线理发育,线理走向和糜棱面理走向基本一致,线理在xy面上的侧伏角绝大多数<30°;该期韧性变形是以左行走滑运动为主。晚期韧性变形中a线理发育,线理倾伏向和糜棱岩中糜棱面理倾向相近,线理在xy面上侧伏角主要在45°～90°之间;该期韧性变形是伸展作用的产物。医巫闾山中生代两期韧性剪切变形作用表明,在侏罗纪至早白垩世期间辽西地区不仅发生了强烈挤压推覆作用和伸展作用,也发生了大规模左行走滑作用。该韧性变形作用的发现对进一步研究辽西中生代的构造演化序列、期次和构造格架转换等问题有重要意义。     

Overburden deformation associated with halokinesis in the Southern North Sea: implications for the origin of the Silverpit Crater

Gravitational collapse in response to the creation of salt swells and diapirs is a common phenomenon within regions such as the Southern North Sea. Although collapse faulting and slumping of linear salt swell flanks has previously been documented, the existence of concentric collapse structures surrounding diapirs and isolated salt lows is a recently recognised feature. 3-D seismic data from the Southern North Sea demonstrates that concentric collapse faulting around both diapirs and subcircular salt lows is common. The recognition of concentric collapse structures formed in response to salt withdrawal, and adjacent inflation, provides an alternative mechanism for the origin of the proposed Silverpit impact crater.     

L'accident du Toulourenc : une limite tectonique entre la plate-forme provençale et le Bassin vocontien à l'Aptien–Albien (SE France)

The WNW–ESE trending Toulourenc Fault Zone (TFZ) is the western segment of the major Ventoux–Lure Fault Zone, which separates the Provençal platform from the Baronnies Vocontian Basin. The TFZ was subject to polyphased Mid-Cretaceous movements, during the Early Aptian and Middle–Late Albian times. The latter faulting episode generated conglomerates and olistoliths resulting from dismantled faultscarps cutting Barremian–Bedoulian limestones. The deformation is related to compressional wrench faulting (NE–SW sinistral faults; dextral component for the TFZ). It induced the uplift of the northwestern corner of the platform, as indicated by a mid-Cretaceous hiatus (Early Aptian pro parte to Early Albian) narrowly delimited in space. The opening of submeridian grabens within the platform favoured the northward transit of channelised coarse-grained Albian sands originating from a southern area. To cite this article: C. Montenat et al., C. R. Geoscience 336 (2004).     

Coastal neotectonics in Southern Central Andes: uplift and deformation of marine terraces in Northern Chile (27°S)

Neotectonic observations allow a new interpretation of the recent tectonic behaviour of the outer fore arc in the Caldera area, northern Chile (27°S). Two periods of deformation are distinguished, based on large-scale Neogene to Quaternary features of the westernmost part of the Coastal Cordillera: Late Miocene to Early Pliocene deformations, characterized by a weak NE–SW to E–W extension is followed by uppermost Pliocene NW–SE to E–W compression. The Middle Pleistocene to Recent time is characterized by vertical uplift and NW–SE extension. These deformations provide clear indications of the occurrence of moderate to large earthquakes. Microseismic observations, however, indicate a lack of shallow crustal seismicity in coastal zone. We propose that both long-term brittle deformation and uplift are linked to the subduction seismic cycle.