Near the border zone an important string of nickeliferous peridotites is emplaced.
交界带上有重要的一连串的含镍橄榄岩(体)的侵入。
Near the border zone an important string of nickeliferous peridotites is emplaced.
交界带上有重要的一连串的含镍橄榄岩(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.
橄榄岩虽然发生了强烈蛇纹岩化(现为蛇纹岩),但蛇纹岩中保
了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.
摘要该蛇绿岩带的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,典型蛇绿岩剖面中的洋壳单元。
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
化(现在为蛇纹
),但蛇纹
中保
了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.
摘要该蛇绿带的
体由地幔橄榄
组成,主要
石类型是方辉橄榄
和纯橄榄
,缺少典型蛇绿
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的一连串的含镍(体)的
。
Peridotite has undergone strong serpentinization and was completely replaced by serpentinite, but the pseudomorph of olivine and orthopyroxene still are preserved.
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
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
组成,主要
石类型是方辉
和纯
,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的一连串的含镍橄榄岩(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.
橄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.
摘要该蛇绿岩带的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,缺少典型蛇绿岩剖面中的洋。
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的一连串的含镍榄
(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.
榄
虽然发生了强烈
纹
化(现在为
纹
),
纹
中保
了斜方辉
榄
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.
摘要该绿
带的
体由地幔
榄
组成,主要
类型是方辉
榄
纯
榄
,缺少典型
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的一连串的含镍橄
(
)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.
摘该蛇绿
带的
由地幔橄
组
,
石类型是方辉橄
和纯橄
,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,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串
含镍
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.
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
石和
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
榄岩组成,主要岩石类型是
榄岩和纯
榄岩,缺少典型蛇绿岩剖面中
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要的一连串的含镍(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.
虽然发生了强烈蛇
化(现在为蛇
),
蛇
中保
了斜方辉石
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
组成,主要
石类型是方辉
纯
,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
,
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生,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。