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1.ARCHAEAN GABBRO INTRUSION IN JINCHANGYU-WANGCHANG AREA, EASTERN HEBEI, CHINA
冀东金厂峪—王厂地区太古代变质辉长岩的基本特征收藏指正
2.another is that of metamorphic peridotite +pyroxenite+gabbro (abbreviated to PPG series).
另一类则是变质橄榄岩+辉石岩+辉长岩岩石组合(简称PPG系列)。收藏指正
3.igneous rock that has solidified beneath the earth's surface; granite or diorite or gabbro.
已经在地表凝固的火成岩;花岗岩、闪长岩或辉长岩的。收藏指正
4.STRUCTURAL MATERIAL PECULIARITIES AND EVOLUTION OF GABBRO ANORTHOSITE COMPLEXES OF THE ALDEN MASSIF, SOUTH RUSSIA
俄罗斯阿尔丹地块南部辉长-斜长岩杂岩体的构造-物质组分特点及其演化收藏指正
5.FLASER—LENTICULAR BEDDINGS IN CARBONATE ROCKS OF THE UPPER PRECAMBRIAN GAOYUZHUANG FORMATION IN THE MING TOMBS AREA,BEIJING
北京十三陵上前寒武系高于庄组碳酸盐岩中的压扁-透镜状层理收藏指正
6.LA-ICPMS Zircon U-Pb Dating of Gabbro from the Bayingou Ophiolite in the Northern Tianshan Mountains
北天山巴音沟蛇绿岩形成于早石炭世:来自辉长岩LA-ICPMS锆石U-Pb年龄的证据收藏指正
7.On the basis of the single factor dry rodded test of coarse aggregate, the optimal framework structure of gabbro Sup-16 gradation is given out.
根据粗集料的单因素捣实试验,确定了辉长岩Sup-16级配骨架最优结构。收藏指正
8.The Kalarsky massif is a constituent part of the extensive Djugdjur Kalarsky gabbro anorthosite belt, confined to the southern periphery of the Aldan massif.
Kalarsky岩体是沿阿尔丹南部边缘分布的规模巨大的Djugdjur?Kalarsky辉长-斜长岩岩带的一部分。收藏指正
9.These deposits were, when being formed, controlled by volcanic structures (volcanic dome and volcanic breccia pipe), fault structures (NE and NW trending), gabbro porphyrite body and “depression in depression”.
火山穹窿、爆发角砾岩筒等火山构造 ,NE向、NW向断裂构造 ,辉石闪长玢岩体 ,“洼中洼”环境等对成矿具有控制作用。收藏指正
10.The dark-gray traction current deposits belong to internal-tide deposits, it develops sandstones and siltsands, and charactered with lenticular, wave, flaser bedding, bimodal cross-bedding and ripple mark.
深水牵引流沉积为内潮汐沉积类型,岩性为细砂岩、粉砂岩,以发育透镜状、波状、脉状层理、双向交错层理、波痕等沉积构造为特征。收藏指正
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