Metamorphism of the Central Anatolian Crystalline Complex, Turkey: influence of orogen-normal collision vs. wrench-dominated tectonics on P–T–t paths     

D. L. Whitney  C. Teyssier  Y. Dilek  A. K. Fayon 《Journal of Metamorphic Geology》2001,19(4):411-432

The Central Anatolian Crystalline Complex (CACC) is a microcontinent in the Alpine–Himalayan belt. It has previously been considered as a coherent structural entity, but, although the entire CACC is comprised of similar rocks (primarily metasedimentary rocks and granitoids), it consists of at least four tectonic blocks characterized by different P–T–t paths. These blocks are the K?r?ehir (north‐west), Akda? (north‐east), Ni?de (south) and Aksaray (west) massifs. The northern massifs experienced thrusting and folding during collision and were slowly exhumed by erosion; metamorphic rocks are characterized by clockwise P–T paths at moderate P–T and local low‐P–high‐T (LP–HT) overprinting in the highest grade rocks. Apatite fission track ages are Eocene to Oligocene (47–32 Ma). The Aksaray block represents the hot, shallow mid‐crust of a Late Cretaceous–early Tertiary arc. It is dominated by intrusions; rare metapelitic rocks record low‐P (< 4 kbar) regional metamorphism overprinted by LP–HT contact metamorphism. Apatite fission track ages are 50–45 Ma. The Ni?de massif is different from the other CACC blocks because it evolved as a core complex in a wrench‐dominated setting. It is characterized by clockwise P–T paths at moderate P–T followed by widespread LP–HT metamorphism. Apatite fission track ages are Miocene (12–9 Ma), significantly younger than those in the northern massifs. Ni?de rocks resided in the mid‐crust at a time when the rest of the CACC was at or near the Earth's surface. Variations in P–T–t and tectonic histories — especially timing of exhumation — between the northern and southern CACC reflect the difference between head‐on collision vs. mid‐crustal wrenching.  相似文献   

三峡水库区危岩防治技术   总被引：15，自引：1，他引：14  

陈洪凯  唐红梅 《中国地质灾害与防治学报》2005,16(2):105-110

危岩是三峡水库区重要的地质灾害类型之一。基于多年来对三峡水库区危岩研究和防治实践,遵循坠落式危岩、滑塌式危岩和倾倒式危岩的危岩失稳分类方案,构建了危岩防治必须坚持防治工程的宏观综合性与危岩体的微观综合性相结合、具备支撑条件时优先采用支撑技术、谨慎使用清除技术、主动防治和被动防护相结合的防治理念。概化提出了支撑、锚固、封填、灌浆、排水和清除共6类主动防治技术,拦石墙、拦石栅栏和森林防护共3类被动防护技术以及锚固一拦挡、锚固一支撑共2类主动一被动联合防治技术。详细论述了每类防治技术的技术要点。该研究成果丰富了重庆市地方标准《地质灾害防治工程设计规范》的技术内涵,对于提高三峡水库区危岩灾害的防治水平有重要价值。  相似文献   

The Higo metamorphic complex in Kyushu, Japan as the fragment of Permo–Triassic metamorphic complexes in East Asia     

Y. Osanai  M. Owada  A. Kamei  T. Hamamoto  H. Kagami  T. Toyoshima  N. Nakano  T.N. Nam 《Gondwana Research》2006,9(1-2):152

The Higo terrane in west-central Kyushu Island, southwest Japan consists from north to south of the Manotani, Higo and Ryuhozan metamorphic complexes, which are intruded by the Higo plutonic complex (Miyanohara tonalite and Shiraishino granodiorite).The Higo and Manotani metamorphic complexes indicate an imbricate crustal section in which a sequence of metamorphic rocks with increasing metamorphic grade from high (northern part) to low (southern part) structural levels is exposed. The metamorphic rocks in these complexes can be divided into five metamorphic zones (zone A to zone E) from top to base (i.e., from north to south) on the basis of mineral parageneses of pelitic rocks. Greenschist-facies mineral assemblages in zone A (the Manotani metamorphic complex) give way to amphibolite-facies assemblages in zones B, C and D, which in turn are replaced by granulite-facies assemblages in zone E of the Higo metamorphic complex. The highest-grade part of the complex (zone E) indicates peak P–T conditions of ca. 720 MPa and ca. 870 °C. In addition highly aluminous Spr-bearing granulites and related high-temperature metamorphic rocks occur as blocks in peridotite intrusions and show UHT-metamorphic conditions of ca. 900 MPa and ca. 950 °C. The prograde and retrograde P–T evolution paths of the Higo and Manotani metamorphic complexes are estimated using reaction textures, mineral inclusion analyses and mineral chemistries, especially in zones A and D, which show a clockwise P–T path from Lws-including Pmp–Act field to Act–Chl–Epi field in zone A and St–Ky field to And field through Sil field in zone D.The Higo metamorphic complex has been traditionally considered to be the western-end of the Ryoke metamorphic belt in the Japanese Islands or part of the Kurosegawa–Paleo Ryoke terrane in south-west Japan. However, recent detailed studies including Permo–Triassic age (ca. 250 Ma) determinations from this complex indicate a close relationship with the high-grade metamorphic terranes in eastern-most Asia (e.g., north Dabie terrane) with similar metamorphic and igneous characteristics, protolith assembly, and metamorphic and igneous ages. The north Dabie high-grade terrane as a collisional metamorphic zone between the North China and the South China cratons could be extended to the N-NE along the transcurrent fault (Tan-Lu Fault) as the Sulu belt in Shandong Peninsula and the Imjingang belt in Korean Peninsula. The Higo and Manotani metamorphic complexes as well as the Hida–Oki terrane in Japan would also have belonged to this type of collisional terrane and then experienced a top-to-the-south displacement with forming a regional nappe structure before the intrusion of younger Shiraishino granodiorite (ca. 120 Ma).  相似文献   

与陆-陆碰撞作用相关的盆-山构造数值模拟   总被引：2，自引：0，他引：2  

崔军文  史金松  李朋武  张晓卫  郭宪璞  丁孝忠 《地球学报》2006,27(1):13-24

陆-陆碰撞作用是导致大陆岩石圈各种地质作用发生的最重要的驱动机制,如何识别和标定陆-陆碰撞作用,特别是其四维时空演化,是地学界长期以来关注和研究的重点。陆-陆碰撞作用的主要表现形式为下伏地块沿陆内俯冲带的强烈下插(俯冲)和上覆地块沿陆内俯冲带的不断仰冲(逆冲扩展),在垂直俯冲带方向出现盆-山相间的构造格局和MOHO的弯曲、错断。通过数值模拟计算,详细论述了在仰冲(逆冲扩展)和俯冲作用过程中,盆地坳陷、山体抬升、MOHO上抬和下坳等各种位移量和位移速率之间的耦合关系及盆地中心的迁移规律。说明它们有可能成为判断或标定陆-陆碰撞作用的一种标志或尺度。  相似文献   

A first-overtone RR Lyrae star with cyclic period changes     

A. Derekas  L. L. Kiss  A. Udalski  T. R. Bedding  K. Szatmáry 《Monthly notices of the Royal Astronomical Society》2004,354(3):821-826

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Extinction map of the Galactic centre: OGLE-II Galactic bulge fields     

Takahiro Sumi 《Monthly notices of the Royal Astronomical Society》2004,349(1):193-204

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Geological significance of seismic reflections in collision belts   总被引：2，自引：0，他引：2  

C. Bois 《Geophysical Journal International》1991,105(1):55-69

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The analysis of indexed astronomical time series – IX. A period change test     

Chris Koen  Fred Lombard 《Monthly notices of the Royal Astronomical Society》2004,353(1):98-104

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A three-dimensional code for muon propagation through the rock: MUSIC     

P. Antonioli  C. Ghetti  E.V. Korolkova  V.A. Kudryavtsev  G. Sartorelli 《Astroparticle Physics》1997,7(4):357-368

We present a new three-dimensional Monte-Carlo code MUSIC (MUon SImulation Code) for muon propagation through the rock. All processes of muon interaction with matter with high energy loss (including the knock-on electron production) are treated as stochastic processes. The angular deviation and lateral displacement of muons due to multiple scattering, as well as bremsstrahlung, pair production and inelastic scattering are taken into account. The code has been applied to obtain the energy distribution and angular and lateral deviations of single muons at different depths underground. The muon multiplicity distributions obtained with MUSIC and CORSIKA (Extensive Air Shower simulation code) are also presented. We discuss the systematic uncertainties of the results due to different muon bremsstrahlung cross-sections.  相似文献   

Three-dimensional V_P and V_S structural models associated with the active subduction and collision tectonics in the Taiwan region     

Kwang-Hee Kim  Jer-Ming Chiu  Jose Pujol  Kou-Cheng Chen  Bor-Shouh Huang  Yih-Hsiung Yeh  Peng Shen 《Geophysical Journal International》2005,162(1):204-220

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