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subduction zone相关的网络例句

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与 subduction zone 相关的网络例句 [注:此内容来源于网络,仅供参考]

Actinolite and pyroxene phenocrysts separated respectively, from chlorite-actinolite schist and altered pillow basalt in the E'rou area of the eastern part of the Shuanghu-Longmuco suture zone, yield well-defined 40Ar/39Ar plateau ages of 235.9±2.6 Ma and 232.5±2.4 Ma. These nearly identical ages are interpreted as defining the age of the tectonothermal event of subduction-related collision along the Shuanghu-Longmuco suture zone.

在藏北龙木错-双湖缝合带东段双湖鄂柔地区,获得绿泥阳起石片岩中阳起石矿物的40Ar/39Ar坪年龄为(235.9±2.6)Ma和枕状玄武岩中蚀变辉石斑晶的40Ar/39Ar坪年龄为(232.5±2.4)Ma,两个年龄具有极好的一致性,记录了中三叠世晚期-晚三叠世早期沿龙木错-双湖缝合带发生俯冲碰撞作用的构造-热事件。

Intermediate and deep focus earthguakes ; Earthquake cycle ; Subduction zone ; Magma tide.

中源和深源地震;地震轮回;俯冲带;岩浆潮。

Great progress has been made in some "hot spot" areas of the geoscientific research, such as the Tibetan plateau, the western Pacific subduction zone, the North China Craton and the South-north seismic belt.

笔者对青藏高原、西太平洋俯冲带、华北克拉通和南北地震带等地区多年来一直存在争议的几个重要地学问题进行了简要的总结,并从地震学的角度出发,对问题的解决提出了粗浅的见解与看法。

Similarly, any pushing force great enough to buckle a plate and form a new trench and subduction zone would certainly form one immediately adjacent to an existing spreading center.

同样,任何大得足以使板块发生挠曲并形成一个新的海沟和俯冲带的推力,也当然会很快在一个现有扩展中心附近形成海沟和俯冲带。

The regions which good quality jadeites should be determined by the four constraints as fellows: 1. In the subduction or collision zone; 2. In the ultrabasic rock bodies especia1ly in duniue bodies; 3. HP~UHP metamorphism zone; 4. Long duration deformation and metamorphism after rock forming.

优质翡翠的成矿预测与找矿靶区的确定应是符合以下四个条件的地区,即:a俯冲带或碰撞带内;b超基性岩体主要是纯榄橄岩体内;c高压与超高压区;d后期发生过长期的动力变质变形作用。

Direct observations and measurements on deformational and sedimentary structures, fluid activities, physical properties, and chemical compositions of core samples from accretionary prisms at different pressure and temperature settings are critical to understanding seismogenic mechanisms of subduction zone earthquakes.

对增生楔不同压力-温度条件下的构造变形、流体活动、沉积特征、岩石物性和化学组成等多方面的直接观测,可以帮助分析俯冲带地震的蕴育和发生的环境与机理。

The closing of the Yaluzangbu suture zone during Oligocene to Miocene and the intracontinental subduction towards to north of the Indian plate occurred in Himalayan piedmont zone during Pliocene to Pleistocene, caused the Himalayan mountain uplifting highly and the Henghe foredeep settling deeply.

3通过塔西南拗陷、库车拗陷、川西拗陷、准噶尔南缘拗陷中新生界构造演化、地层沉积、烃源岩特征、形变特征的类比分析,将库车拗陷、准噶尔南缘拗陷划分为弱压扭盆地;塔西南拗陷、川西拗陷划分为强压扭盆地。

Kalamaili suture zone is an important plate boundary in north Xinjiang, and there are plenty of Neopaleozoic volcanic rocks around itThese volcanic rocks are enriched in LILEs and relatively depleted in HFSEs, and they are also characterized by high Nb, Zr, TiO2 contents and Zr/Y, Nb/Y ratios, and depleted SrNd isotopesThe characteristics of these volcanic rocks suggest that they were produced in postcollisional periodThe postcollisional volcanic rocks around Kalamaili suture zone become younger from west to east, which indicates that this suture zone entered postcollisional period gradually from west to east, and reflects that the Kalamaili Ocean had been closed gradually from west to eastAs to the Kalamaili suture zone in postcollisional period, the lithosphere extended and thinned, and the asthenosphere materials upwelled and melted partially, and intensive mantle convection occurred, leading to a plenty of mantlederived magmas underplating the suture zoneThe lithospheric mantle metasomatized by fluid in subduction period melted partially under decompression and high temperature, the resulting melts contaminated the underplating asthenospheric materials, and the erupted lavas became the Neopaleozoic postcollisional volcanic rocks

卡拉麦里缝合带是北疆的一条重要界线,沿该带广泛发育晚古生代火山岩。这些火山岩具有LILE相对富集、HFSE相对亏损的特征,且具有较高的Nb、Zr、TiO2含量和Zr/Y、Nb/Y比值,SrNd同位素主要表现出亏损的特征。综合分析表明,这些火山岩形成于后碰撞期。对卡拉麦里缝合带而言,从西向东后碰撞火山岩的时代逐渐变新,表明该缝合带从西向东逐渐演化进入后碰撞期,这从侧面反映了卡拉麦里洋盆是从西向东逐渐关闭的。对卡拉麦里缝合带而言,在后碰撞期,岩石圈伸展减薄,软流圈地幔物质上涌并发生部分熔融,加上地幔对流作用强烈,使得缝合带下产生了大规模的幔源岩浆底垫;先前在洋壳消减期被流体交代提取过的岩石圈地幔也在低压高温下发生部分熔融,形成的熔体混染了底垫的软流圈物质并喷发,形成了晚古生代的后碰撞期火山岩。

The metamorphic peridotites display SiO2 (39.08%~40.45%),TiO2 (0.02%~0.03%), Mg′(87.10~90.33). The metamorphic gabbros show geochemical characteristics of enriched in LILE, and depleted in HFSE. Furthermore, there are some high-Mg diorites exposed. In summary, the Daomaoqi ophiolitic mélange formed in a supra-subduction zone.

其中,变质橄榄岩类SiO2含量为39.08%~40.45%,TiO2含量为0.02%~0.03%,Mg′为87.10~90.33,;变质辉长岩表现为大离子亲石元素K、Rb、Sr、Ba明显富集,高场强元素Nb、Ta、Zr相对亏损,以及高镁闪长岩的出露都与SSZ型蛇绿岩特点相符。

Verde Basin is a marginalforeland basin genetically related to the Ouachita overthrust 'belt and its as ociated subduction zone.

佛得角盆地是marginalforeland盆地基因有关沃希托覆'带和其作为ociated俯冲带。

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