syntexis [sin'teksis]

syntexis的基本解释

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[医] 消瘦, 同熔作用

与syntexis相关的网络例句 [注：此内容来源于网络，仅供参考]

Nd-Sr isotopic compositions for 20 granitoid bodies of syntexis series in South China have been studied in this paper.

本文讨论了华南20个同熔系列花岗岩类的Nd-Sr同位素组成。

Based on the isotopic compositions of samples and their distribution characteristics on the _-T,~(87Sr/~(86)Sr_i-T, and _-_ diagrams, these granitoids of syntexis series are considered as mixing products of upper crust end-member and depleted mantle end-member in certain proportion.

根据样品的同位素组成及其在￠Nd-T，(87Sr/86Sr)i-T和￠Nd-￠Sr图上的分布特征，认为这些同熔系列花岗岩类是华南上地壳端员和亏损地幔端员按一定比例混合的产物。

The material for formation of the granitoids isderived from mixing sources of crust and mantle, with decreasing in crust-derived componentsfrom early to late.5. The tectonic setting for formation of the Mesozoic granitoids in the region isdefined as a post-collisional setting. The occurrence of a small part of rocks with characteristics ofcollisional or anorogenic granitoids provides evidence for the continuous process oftransformation of tectonic regime from collisional through post-collisional to anorogenic.6. Themultiple cycles of mantle-derived magma underplating caused by the multiple stages oflithospheric thinning in the Mesozoic result in the partial melting of middle to lower crust orcrust-mantle syntexis to form magmas. The crystallization of these magmas emplacing afterfractionation is responsible for the formation of the Mesozoic granitoids in this region.

形成花岗岩类的成岩物质来自壳幔混源。5、河南省西部地区中生代花岗岩类成岩构造环境为碰撞后环境，部分岩石具有碰撞期或非造山期花岗岩的某些特征，表明碰撞后阶段既是碰撞造山过程的延续，又是向非造山环境的构造转换时期，因而其岩浆活动在一定程度上仍然继承了碰撞前消减时期和碰撞时期已经活化的岩浆源区性质。6、研究表明，区内中生代多阶段的岩石圈减薄作用引发多旋回的幔源岩浆底侵以及中下地壳的部分熔融或壳幔同熔，由此形成的岩浆经分异演化后侵位可以形成区内的中生代花岗岩类。

与syntexis相关的网络解释 [注：此内容来源于网络，仅供参考]

syntexis：同熔酌

syntectonic recrystallization 同构造再结晶 | syntexis 同熔酌 | synthectic mineral 合成矿物

syntexis：消瘦

synovium 滑膜 | syntexis 消瘦 | synthetic antigen 合成抗原

syntexis：同熔作用

syntectic /同熔作用/ | syntexis /同熔作用/ | synthal /合成橡胶/

syntexis：共熔

syntan 合成单宁 | syntexis 共熔 | synthesis 合成