Near the border zone an important string of nickeliferous peridotites is emplaced.
在靠近交界有重要的一连串的含镍
榄岩(体)的侵入。
Near the border zone an important string of nickeliferous peridotites is emplaced.
在靠近交界有重要的一连串的含镍
榄岩(体)的侵入。
Peridotite has undergone strong serpentinization and was completely replaced by serpentinite, but the pseudomorph of olivine and orthopyroxene still are preserved.
榄岩虽然发生了强烈蛇纹岩化(现在为蛇纹岩),但蛇纹岩中保
了斜方辉石
榄石的假象。
The Ophiolite massifs are composed of mantle peridotite that is mainly harzburgite and dunite, and lacked of crust magmatite within the typical Ophiolite suite.
摘要该蛇绿岩的岩体由地幔
榄岩组成,主要岩石类型是方辉
榄岩
榄岩,缺少典型蛇绿岩剖面中的洋壳单元。
声明:以例句、词性分类均由互联网资源自动生成,部分未经过人工审核,其表达内容亦不代表本软件的观点;若发现问题,欢迎向我们指正。
Near the border zone an important string of nickeliferous peridotites is emplaced.
在靠近交有重要的一连串的含镍
岩(体)的侵入。
Peridotite has undergone strong serpentinization and was completely replaced by serpentinite, but the pseudomorph of olivine and orthopyroxene still are preserved.
岩虽然发生了强烈蛇纹岩化(现在为蛇纹岩),但蛇纹岩中保
了斜方辉石和
石的假象。
The Ophiolite massifs are composed of mantle peridotite that is mainly harzburgite and dunite, and lacked of crust magmatite within the typical Ophiolite suite.
摘要该蛇绿岩的岩体由地幔
岩组成,主要岩石类型是方辉
岩和
岩,缺少典型蛇绿岩剖面中的洋壳单元。
声明:以例句、词性分类均由互联网资源自动生成,部分未经过人工审核,其表达内容亦不代表本软件的观点;若发现问题,欢迎向我们指正。
Near the border zone an important string of nickeliferous peridotites is emplaced.
在靠带上有重要的一连串的含镍橄
(体)的侵入。
Peridotite has undergone strong serpentinization and was completely replaced by serpentinite, but the pseudomorph of olivine and orthopyroxene still are preserved.
橄虽然发生了强烈蛇纹
化(现在为蛇纹
),但蛇纹
中保
了斜方辉石和橄
石的假象。
The Ophiolite massifs are composed of mantle peridotite that is mainly harzburgite and dunite, and lacked of crust magmatite within the typical Ophiolite suite.
摘要该蛇绿带的
体由地幔橄
组成,主要
石类型是方辉橄
和纯橄
,
少典型蛇绿
剖面中的洋壳单元。
声明:以上例句、词性分类均由互联网资源自动生成,部分未经过人工审核,其表达内容亦不代表本软件的观点;若发现问题,欢迎向我们指正。
Near the border zone an important string of nickeliferous peridotites is emplaced.
在靠近交界带上有重要一连串
含镍橄榄岩(体)
侵入。
Peridotite has undergone strong serpentinization and was completely replaced by serpentinite, but the pseudomorph of olivine and orthopyroxene still are preserved.
橄榄岩虽然发生了强烈蛇纹岩化(现在为蛇纹岩),但蛇纹岩保
了斜方辉石和橄榄石
假象。
The Ophiolite massifs are composed of mantle peridotite that is mainly harzburgite and dunite, and lacked of crust magmatite within the typical Ophiolite suite.
摘要该蛇绿岩带岩体由地幔橄榄岩组成,主要岩石类型是方辉橄榄岩和纯橄榄岩,缺少典型蛇绿岩剖
洋壳单元。
声明:以上例句、词性分类均由互联网资源自动生成,部分未经过人工审核,其表达内容亦不代表本软件观点;若发现问题,欢迎向我们指正。
Near the border zone an important string of nickeliferous peridotites is emplaced.
在靠近交界带上有重的一连串的含镍橄榄
(体)的侵入。
Peridotite has undergone strong serpentinization and was completely replaced by serpentinite, but the pseudomorph of olivine and orthopyroxene still are preserved.
橄榄虽然发生了强烈蛇纹
(
在为蛇纹
),但蛇纹
中保
了斜方辉石和橄榄石的假
。
The Ophiolite massifs are composed of mantle peridotite that is mainly harzburgite and dunite, and lacked of crust magmatite within the typical Ophiolite suite.
该蛇绿
带的
体由地幔橄榄
组成,主
石类型是方辉橄榄
和纯橄榄
,缺少典型蛇绿
剖面中的洋壳单元。
声明:以上例句、词性分类均由互联网资源自动生成,部分未经过人工审核,其表达内容亦不代表本软件的观点;若发问题,欢迎向我们指正。
Near the border zone an important string of nickeliferous peridotites is emplaced.
在靠近交界带上有重要一连串
含镍橄榄
(
)
侵入。
Peridotite has undergone strong serpentinization and was completely replaced by serpentinite, but the pseudomorph of olivine and orthopyroxene still are preserved.
橄榄虽
了强烈蛇纹
化(现在为蛇纹
),但蛇纹
中保
了斜方辉石和橄榄石
假象。
The Ophiolite massifs are composed of mantle peridotite that is mainly harzburgite and dunite, and lacked of crust magmatite within the typical Ophiolite suite.
摘要该蛇绿带
由地幔橄榄
组成,主要
石类型是方辉橄榄
和纯橄榄
,缺少典型蛇绿
剖面中
洋壳单元。
声明:以上例句、词性分类均由互联网资源自动成,部分未经过人工审核,其表达内容亦不代表本软件
观点;若
现问题,欢迎向我们指正。
Near the border zone an important string of nickeliferous peridotites is emplaced.
在靠近交界带上有重要一连串
含镍橄榄
(
)
侵入。
Peridotite has undergone strong serpentinization and was completely replaced by serpentinite, but the pseudomorph of olivine and orthopyroxene still are preserved.
橄榄虽
了强烈蛇纹
化(现在为蛇纹
),但蛇纹
中保
了斜方辉石和橄榄石
假象。
The Ophiolite massifs are composed of mantle peridotite that is mainly harzburgite and dunite, and lacked of crust magmatite within the typical Ophiolite suite.
摘要该蛇绿带
由地幔橄榄
组成,主要
石类型是方辉橄榄
和纯橄榄
,缺少典型蛇绿
剖面中
洋壳单元。
声明:以上例句、词性分类均由互联网资源自动成,部分未经过人工审核,其表达内容亦不代表本软件
观点;若
现问题,欢迎向我们指正。
Near the border zone an important string of nickeliferous peridotites is emplaced.
在靠近交界上有重要的一连串的含镍橄榄
(体)的侵入。
Peridotite has undergone strong serpentinization and was completely replaced by serpentinite, but the pseudomorph of olivine and orthopyroxene still are preserved.
橄榄虽然发生
蛇纹
化(现在为蛇纹
),但蛇纹
中保
斜方辉石和橄榄石的假象。
The Ophiolite massifs are composed of mantle peridotite that is mainly harzburgite and dunite, and lacked of crust magmatite within the typical Ophiolite suite.
摘要该蛇的
体由地幔橄榄
组成,主要
石类型是方辉橄榄
和纯橄榄
,缺少典型蛇
剖面中的洋壳单元。
声明:以上例句、词性分类均由互联网资源自动生成,部分未经过人工审核,其表达内容亦不代表本软件的观点;若发现问题,欢迎向我们指正。
Near the border zone an important string of nickeliferous peridotites is emplaced.
在靠近交界有重要的一连串的含镍
榄岩(体)的侵入。
Peridotite has undergone strong serpentinization and was completely replaced by serpentinite, but the pseudomorph of olivine and orthopyroxene still are preserved.
榄岩虽然发生了强烈蛇纹岩化(现在为蛇纹岩),但蛇纹岩中保
了斜方辉石
榄石的假象。
The Ophiolite massifs are composed of mantle peridotite that is mainly harzburgite and dunite, and lacked of crust magmatite within the typical Ophiolite suite.
摘要该蛇绿岩的岩体由地幔
榄岩组成,主要岩石类型是方辉
榄岩
榄岩,缺少典型蛇绿岩剖面中的洋壳单元。
声明:以例句、词性分类均由互联网资源自动生成,部分未经过人工审核,其表达内容亦不代表本软件的观点;若发现问题,欢迎向我们指正。