海绿石

The Glauconite Sandstone is a persistent stratigraphic unit.

海绿石砂岩是一个稳定的地层单元。

Glauconite, detrital carbonate skeletal debris, marine fossils, and collophane are commonly present.

海绿石、碳酸盐骨骸碎屑、海相化石和胶磷矿普遍出现。

An olive-green sandstone containing glauconite.

一种橄榄绿的砂岩，含海绿石。

A glass of fresh, fruity white accompanying vegetables previously marinaded in olive oil and served grilled, set down on a stone table in a shady spot in the garden situated high in the hills of the islandof Ischia ;The exilarating view of a vineyard nestled between the sea and the mountains during a walk around the sharp schistous terrasses of Banyuls ;The gentle pleasure of cycling in the Entre-Deux-Mers, along the delightful Roger Lapbérie bicycle track ;The magical encounter with a wiley, entertaining wine grower in the cool of his Burgundian cellar ;All this and many other happy holiday memories evoked by the wines themselves which were bought as souvenirs...This Summer, we hope you will also taste the thousand and one pleasures of the 'wine civilization'!

一杯鲜活、果味浓郁的白葡萄酒，配予浸过橄榄油的烤蔬菜；置于Ischia岛顶端绿木遮挡的公园石桌上；在Banyuls陡峭的平台上漫步时陶醉在海与山之间的葡萄园美景；沿着Roger-Lapébie自行车道（以原环法自行车赛冠军命名）骑车畅游在两海之间；在勃艮第清凉的酒窖内与狡诈的酿酒人相遇；以及其它等多在假期中以葡萄酒为证的美好回忆……今年夏天，我们预祝您度过一段品味葡萄酒文明的美好时光！

The Phanerozoic glauconites in this study show that they were formed in an environment of weak reduction and low sedimentation.

显生宙的海绿石，多年来研究的结果表明海绿石发育在慢速弱还原环境。

Rigid coral branches present the illusion of fluid movement in a turquoise sea near the Turks and Caicos Islands.

硬珊瑚分支目前的假象流体运动在绿松石海靠近特克斯和凯科斯群岛。

Blue sky and turquoise blue sea meet…. the skyline at my hometown is so very beautiful

蓝色的天空和绿松石般的海洋相衬……祖国的大好河山真是美啊。

Results show that the Spiti shale in Zanskar terminated 15Ma later than that in southern Tibet, while the lowermost Cretaceous quartz sandstone in Zanskar appeared 18Ma later than that in southern Tibet. The age of volcanic sandstone in southern Tibet is very poorly time constraint and their deposition occurred somewhere within Berriasian～early Albian. In Thakkhola, the Chukh Group volcanic sandstone are of late Hauterivian-early Albian age (duration about 20Ma), while in Zanskar, the volcanic sandstones facies only appeared in Albian (duration of less than 10Ma). Therefore, it can be concluded that the onsets of both quartz sandstone and volcanic sandstone occurred earlier in eastern Tethys Himalayas than in western Tethys Himalayas .

侏罗纪末～白垩纪初印度大陆的北缘同时期存在大陆向上挠曲，导致陆源碎屑输入量的快速增加，石英砂岩广泛存在；早白垩世火山岩屑砂岩对应着的印度大陆北缘地层侵蚀加深，使得较深部的深成火山岩暴露并遭受侵蚀；石英砂岩和早白垩世岩屑砂岩所代表的印度大陆剥露时间在空间上的&东早西晚&，说明构造运动首先是从特提斯喜马拉雅的东部开始（大印度与澳大利亚的彻底分离），然后逐渐波及西部的，东西时间差为15～20Ma；由于地壳均衡作用，大陆分离后原先地壳挠曲转变为地壳下沉，发生强烈的构造沉降，故Albian之后沉积一套深水环境下的海绿石、磷酸盐和黑色页岩沉积。

Under certain circumstances, the sea can generate a type of secondary mineral, called glauconitic sandstone.

海洋在一定环境下，会产生一种次生矿，叫海绿石。

An olive-green ''.

一种橄榄绿的砂岩，含海绿石。

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。