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绿泥石

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The alabandite and getchellite of hydrothermal origin, cement anatase of alkaline volcanic origin, and the high content of chlorite in coal were fist found in coals.

在西南地区晚二叠世煤中首次发现了热液成因的硫锰矿和硫砷锑矿、碱性火山灰成因的胶态锐钛矿和陆源碎屑成因的斜绿泥石

Amygdaloidal calcite aggregate and fine stockwork of calcite-prenite-chlorite are superimposed on the asphalt and carbon-rich ores.

在矿体中还见到葡萄石-绿泥石-方解石杏仁体和细网脉,与沥青团块抑或共生抑或稍晚于后者。

Meanwhile, the volcaniclastic rocks were modificated by the thermal fluid activity, for example, sericitization of plagioclase, chloritization of volcanic detritus in andesitic detris tuff; in the tufaceous mud, the thermal fluid activity accelerates "maturating" of the organic carbon by heating; and the trace elements show an anomaly in the wall rocks.

同时,受热流体活动的影响,热流体对火山碎屑岩具有一定改造作用,如在安山质岩屑凝灰岩中,斜长石绢云母化、火山岩岩屑绿泥石化明显;在凝灰质泥岩中,热流体对围岩中有机碳具有明显的&催熟&加热作用,微量元素则出现异常现象。

Chlorite is a common authigenic mineral lining the pores of sandstones.

绿泥石是一种常见的自生矿物,作为砂岩孔隙的内衬。

In some cases, the presence of authigenic chlorite on sand grains can inhibit the growth of pore-filling cements during diagenesis and preserve pore space for occupation by hydrocarbons.

在有些情况下,砂岩颗粒上有自生绿泥石,它可以在成岩作用期间抑制填隙的胶结物生长,并保护油气占据的孔隙空间。

Is around ore shoots to be distribute with symmetry, that show the block and brecciated ores of the Tongmugou zinc deposit are fluid metasomatic reformed deposit.

后生流体交代岩(主要由透闪石、绿帘石、透辉石、黑云母、石英、绿泥石等矿物组成)显著受层间断层控制,它是流体交代原热水沉积层和热水沉积闪锌矿纹层而形成的,该矿床为热水沉积-流体交代改造矿床。

In the Ranger area highly chloritic rocks were believed to be altered dolerites.

兰杰地区的强烈绿泥石化岩石据信可能是蚀变粒玄岩。

With together, the chloritic amphibolites may be a kind of rocks making up the middle crust in northern margin of the North China craton.

综合来看,实验的绿泥石化斜长角闪岩有可能是组成现今华北克拉通北缘的中地壳岩石之一。

The P-wave velocity v(superscript p and electrical conductivity of chloritic amphibolite are measured at 1.0 GPa, from room temperature to 700℃, using ultrasonic reflection-transmission combined method and impedance spectra method respectively. The sample comes from northern margin of the North China craton.

在1.0 GPa、室温至700℃条件下,分别采用超声波反射-投射法和阻抗谱法,测量了华北克拉通北缘绿泥石化斜长角闪岩的弹性波纵波速度和电导率。

Chloritization was one of the mast important alteration types in Nos.

绿泥石化是201和361铀矿床最重要的蚀变类型之一。

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