浅成的

The shoshonites in Zaxue area of Tibet, including the hypabyssal intrusive quartz-monzonite porphyry and the volcanic rocks of Pana Formation, distribute in the central part of Gangdese magmatic belt.

西藏扎雪地区钾玄岩包括浅成侵入的石英二长斑岩和帕那组的火山岩，分布于冈底斯岩浆弧带中段。

Leaf blade oblate to 5-angled or oblate to orbicular-ovate, apex often 3-lobed, base often truncate or subcordate; spikes well branched into subpanicle.

叶片扁球形到具5个角或扁球形到圆形卵形的，先端通常3浅裂的，基部通常截形或近心形；穗状花序多分枝成近圆锥花序 16 B 。

Which were found in succession in the Yili Late Paleozoic volcanic rock province in the north section of West Tianshan Mountains ,are considered as epithermal mineralizing type,and furtherly divided into adular sericite sub type and silicated rock sub type.

20世纪90年代，在新疆西天山北段晚古生代火山岩区内相继发现了阿希大型金矿床及其外围的伊尔曼得、恰布坎卓它等金矿床，并进一步确定了其系产于晚古生代火山岩内的浅成低温矿床。

And therefore the Jinchang gold deposit can be classified as the catalog of mesothermal gold deposits which are related to post-magmatic hydrothermal activity of Mesozoic volcano-subvolcanic magmatism.

矿石中脉石英的Ar-Ar年龄测定结果(119.40～122.53Ma)，表明矿化作用发生于燕山中晚期，矿床成因为与中生代火山-次火山活动有关的岩浆期后浅成中温热液矿床。

The Dongan gold deposit is a great epithermal deposit newly discovered in Heilongjiang province.

东安金矿是黑龙江省发现的大型浅成低温热液低硫化物型金矿床。

The Wufeng-Wuxingshan gold deposit in Yanbian area, Jilin Province is a large epithermal gold deposit of low-sulphidation type.

延边五凤五星山金矿床是一个大型的典型低硫化型浅成低温热液金矿床。

The Wufeng-Wuxingshan gold deposit in Yanbian area, Jilin Province is a large epithermal gold deposit of low-sulphidation type.

延边五凤-五星山金矿床是一个大型的典型低硫化型浅成低温热液金矿床。

The epithermal gold deposits in northern Xinjiang can be divided into high-sulfidation and low-sulfidation types, with the latter being the main type.

文章在总结前人研究成果的基础上，提出新疆北部古生代浅成低温热液型金矿床可以划分为高硫型和低硫型两大类，以后一种为主。

Their distribution districts contain both world-class porphyry copper gold as well as hot-spring gold deposits.

埃达克岩的分布区与世界级斑岩铜－金矿和浅成热泉金矿成矿带分布一致。

This deposit should be porphyry copper deposit, the magmatic rocks related tomineralization mainly include quartz diorite porphyry and granodiorite porphyry. Thedeposit developed in the environment of epi-middle-low temperture.

该矿床为斑岩型铜矿，与成矿有关的岩体为花岗闪长斑岩和石英闪长斑岩，矿床形成于浅成中低温环境。

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。