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岩石圈

与 岩石圈 相关的网络例句 [注:此内容来源于网络,仅供参考]

Evolutionary radiation of the biotas accompanied with a series of geological events, such as lithospheric thinning, magmatic activities, metamorphic core complex and extensional basins, which suggests a mechanism of interaction and response in the Earth surface systems.

它们的快速演变过程和华北克拉通上同时期发育的岩石圈减薄、大面积强烈岩浆活动、变质核杂岩及伴随的伸展盆地等地球表层重大地质事件并行发生,表现着地壳表层系统圈层间的相互作用和响应。

The coherences between Te and the thermal lithospheric thickness, the base depth of magnetic tectonic layer are much better in the whole Transect, these demonstrate Te of continental lithosphere is closely concerned with"heat"geophysical parameters, also prove the heat structure of the lithosphere is the primary factor of influencing the value of Te.

整个断面上热岩石圈厚度、磁性构造层底面深度与Te值的相关性更好。

The southern Yellow Sea has a thicker lithosphere with the characteristics of lower Yangtze craton.

南黄海具有相对较厚的岩石圈,较多地保存了下扬子克拉通的特征。

The Yangtze and ORDOS cratons with thickened lithospheric roots become as a transitional zone or a firm rock in midstream between the eastern and western parts with different structural characteristics in Chinese continent and obstruct mutual material exchange and migration between the both.

扬子克拉通和鄂尔多斯克拉通厚岩石圈根构成了中国东部和西部之间的交接转换带,成为阻挡东/西部物质交换迁移的中流砥柱。

Also,it is an important area of epithermal gold ore-deposits localities.

东南亚地区地处西太平洋构造-岩浆活动带上,是中新生代以来地球岩石圈中最复杂的构造活动区之一,也是全球浅成低温热液金矿床的重要产区之一。

The Ordos craton basin was relatively stable- featured in the following aspects, such as the lithosphere texture, thermal flow, subsidence /sedimentation, and tectonic evolution.

鄂尔多斯克拉通有其稳定的一方面,表现在岩石圈结构、沉积沉降、热流、构造的相对稳定,不仅在克拉通层序的构造沉积稳定,在后期仍然表现为相对稳定。

The outgas types and amount of different gas resource varied with the different geological conditions and evolution processes. There are four outgas models including the model in which inorganic gas directly overflows from mantle matter through lithospheric fracture,the model of heat flow piercement outgas,the model of volcano-magma outgas,and the model of carbonate rock outgas due to heat metamorphism.

对气藏成藏条件和深部壳幔结构的研究表明,松辽盆地存在多种类型无机&气源&,由于赋存的地质条件和演化过程不同,不同气源脱气的方式、脱出气体的类型、脱气量也大不相同,共有4种主要的模式:地幔物质沿超岩石圈断裂直接脱气模式;热流底辟体脱气模式;火山—岩浆成因模式;碳酸盐岩热变质成因模式。

The geochemicl characteristics of western Liaoning Cenozoic lavas and Longgan mantle xenoliths reveal the occurrence and the period of this process in this paper.

在中生代时期,该古老克拉通的下地壳和岩石圈地幔拆沉进入了软流圈地幔,产生了壳-幔之间的物质交换。

Temporal evolution indicates a gradual depletion of mantle sources, which suggests that lavas formed before major lithospheric thinning had occurred.

从时间的角度论证了源区有从略富集逐渐演化为略亏损的趋势,结合区域上的变化,提出这种演化特征反映了苦橄岩是在岩石圈大规模减薄之前形成的。

Plate tectonics; ocean ridge; magmatism; ocean crust; lithosphere; Benioff Zone; Precambrian; seafloor magnetic lineations; mantle; basalt; transform fault; metamorphism; metamorphic facies; Strontium isotope; sulphide ore

关键词:板块构造;洋脊;岩浆作用;洋底壳;岩石圈;贝尼奥夫带;前寒武纪;海底磁性线壮构造;地幔;玄武岩;转换断层;变质作用;变质相;锶同位素;硫化矿

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