METAMO相关论文
有不同变丑机制(易碎的变丑，易碎可锻的变丑，和可锻的变丑) 的煤表示在 macromolecular 的不同方法基于变态组织进化。因为 macromol......
Distinguishable Signature of UHP and Non-UHP Granitic Gneisses in the Sulu Terrane: Evidence from Mi
The pre-pilot drillhole CCSD-PP1 of the Chinese Continental Scientific Drilling Project, with a depth of 432.08 m, is lo......
Crustal Signature of δ~(13)C and Nitrogen Content in Microdiamonds from Erzgebirge, Germany: Ion Mic
The study of δ13CPDB (Pee Dee Belemnite) and nitrogen contents in 1 to 5-μm-diameter microdiamonds included in garnets......
A review of the New Geophysics:a new understanding of pre-fracturing deformation in the crack-critic
This paper reviews a new understanding of shear-wave splitting (seismic-birefringence) that is a fundamental revision of......
Laser Ablation ICP-MS U-Pb Zircon Geochronology of Granitoids and Quartz Veins in the Shihu Gold Min
The Shihu gold deposit, situated in the Taihang Mesozoic orogen of the North China Craton (NCC), is hosted by ductile-br......
介绍里底水电站主要碾压混凝土施工工艺、施工方法和实施成果。里底水电站将碾压混凝土砂石粉含量上限选到24%,适当加大了砂率,使......
介绍了滹沱群与五台岩群区域构造特征：二者片理彼此平行，并不出现“片理不整合”。分析了滹沱群与五台岩群两套地层变质程度协调一致......
阐述了洗精煤在贮存过程中其胶质层厚度及粘结指数随季节变化的规律,该结果有利于指导单种煤采购和煤场管理,也为生产品质稳定的焦......
Pitx2基因被认为是脊椎动物中调节内脏器官左右不对称的关键转录因子。为进一步探讨牙鲆变态期间的左右不对称是否也受Pitx2的左特......
通过对铜陵地区主要铁铜矿床矿石组构研究表明，石炭系统铁铜矿床中存在沉积成岩、热变质及热液充填、交代的矿石组构。结合矿石组分......
采用试验水体中添加化学诱导物的方法研究L-DOPA（L-多巴）对西施舌（Coelomctra antiquata）眼点幼虫附着变态的诱导作用。结果表明，L-DOPA......
详细地阐述了科学钻探的由来、发展状况、钻探的目标和实际意义,介绍了中国大陆科学钻探工程的组织与实施,并详细论述了科钻1井的......
本文对位于青藏高原拉萨地体东南缘林芝杂岩中的片麻岩进行了岩石学和锆石U-Pb年代学研究。所研究的样品包括正片麻岩和副片麻岩,......
球状结构是指由纤维状晶体组成的放射状集合体,其为一种高度不平衡的结构。它们常见于火山岩、假玄武玻璃、沉积岩以及热液沉积物......
为了解决复杂产品虚拟样机模型库管理方法引起的虚拟样机间模型的可复用性低、共享性低、存储不方便等问题,提出了一种基于虚拟样......
Zonal Metamorphic Complex in the Tongulack Mountain Ridge, Altai, Russia, and Explanation of Its Ori
A moderate pressure / high temperature zonal metamorphic complex in the Tongulack Mountain Ridge, Altai, Russia, is desc......
Value delivery is becoming an important asset for an organization due to increasing competition in industry. Therefore, ......
