岩化

Fluid system ; basin's compaction fluid ; dolomitization ; numerical simulation

流体系统；盆地压实流体；白云岩化；数字模拟

The compaction fluid system of Hongyan basin formed Hongyan pyrite ore belt in the old upheaved region that situated at the edge of the basin, and at the same time the impressing dolomitization occurred.

红岩地区盆地压实流体系统在盆缘古隆起地段形成红岩型黄铁矿矿带的同时，还形成特征的白云岩化作用。

Thedevelopment of high quality reservoir has close relationship with dolomite types, atthe same time it appears different geochemical characteristics;In contrast,geochemical characteristics can verify the dolomitization type in turn, which offer theevidences for dolomite diagenic.

优质储层的发育和沉积相、白云岩化类型密切相关，表现出不同的地球化学特征。

Low δ18O of an ancient rock may have been set during the initial lithification event or during a much later metamorphic event.

早期岩石中较低的δ18O比值可以在初期的岩化事件中形成或者后期的变质作用。

Fault gouge ; High temperature and pressure ; Stress-Strain ; Lithification ; Stable sliding ; Earthquake

断层泥；高温高压；应力-应变；岩化；稳定滑动；地震

In this 'lithification' process, the originally precipitated phases undergo dissolution, reprecipitation, and isotopic re-equilibration with ambient pore fluids.

在这个所谓的岩化过程，最初沉淀的沉积物经历了溶解，再沉淀，与周围孔隙中的流体进行的同位素再平衡分馏等过程。

We show that the combined oxygen and carbon isotope systematics are identical to those of well-understood Phanerozoic examples that lithified in coastal pore fluids, receiving a large groundwater influx of photosynthetic carbon from terrestrial phytomass.

他们得出一个引人注目的结论：这些氧和碳同位素的组合体系与我们非常了解的显生宙样品中的相同；显生宙样品岩化在了沿海的孔隙液中，接受着含有来自陆地植物质的光合作用碳的地下水流入。

Formation of augen fabrics is decided by the ductile deference between the porphyroblast and matrix in deformation rock.

长石眼球构造的形成主要是由长石与石英的韧性差决定的，塑性变形首先从斑晶的周围部分开始，逐渐向斑晶发展，脆性残斑核不断减小，这与剪切带内糜棱岩化强度分带相一致。

Formation of augen ...

长石眼球构造的形成主要是由长石与石英的韧性差决定的，塑性变形首先从斑晶的周围部分开始，逐渐向斑晶发展，脆性残斑核不断减小，这与剪切带内糜棱岩化强度分带相一致。

In this process, the crust will be fractionated: the moving down mafic rocks will be eclogitization gradually and thus have a higher density to result in regionally gravitational instability.

在这个过程中，地壳将发生分异，向下迁移的镁铁质物质将由于逐渐榴辉岩化而大大增加自身的密度，导致区域重力不稳定。

The split between the two groups can hardly be papered over.

这两个团体间的分歧难以掩饰。

This approach not only encourages a greater number of responses, but minimizes the likelihood of stale groupthink.

这种做法不仅鼓励了更多的反应，而且减少跟风的可能性。