- 更多网络例句与洋中脊相关的网络例句 [注：此内容来源于网络，仅供参考]
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Well-documented Lu-Hf isotope data from the oceanic basalts show that,the starting area of magma melting for the MORBs derived from the DMM component would be in the the depth of garnet peridotite,i.e.at the depth of 80―90 km instead of less than 60 km,which is at the depth of spinel peridotite as proposed early.The HIMU component,which is characterized by its high rediogenic lead,is refered as a special mantle component differentiated at some time in geological history from the lower mantle.A correlation study of Hf-Nd isotope between the chondrite and oceanic basalts implies that no isolated primitive mantle might have remained.
大量的大洋玄武岩Lu-Hf同位素研究表明：具亏损地幔端元来源的洋中脊玄武岩岩浆部分熔融的初熔区位于石榴石稳定场深度，即深度为80-90 km的石榴石二辉橄榄岩地幔，而不是原来所认为的尖晶石二辉橄榄岩区(深度小于60 km)；以高放射成因Pb为特征的高U地幔端元应代表了下地幔物质在某一特定时期发生分异作用的结果；球粒陨石与大洋玄武岩Hf同位素对比研究表明，没有原始地幔物质能保留至今的迹象。
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The pillow lava, with affinity of MORB, plots in the field of MORB and IAT, suggesting that the Yushigou ophiolite formed in a tectonic setting like the Middle Ocean Ridge and then were changed by volcanic arc magmatism.
地幔橄榄岩主要是方辉橄榄岩，其主要氧化物成分较为单一，具LREE富集、Eu亏损的U形REE配分模式，亏损强不相容元素；枕状熔岩具典型MORB特征，在构造判别图解上位于MORB和IAT区域，指示蛇绿岩可能形成于类似于洋中脊的构造环境，并受到火山弧岩浆作用的影响。
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The existence of MORB type tholeiite depleted in LREE(TH1) demonstrates that some pieces of ocean crust may be involved there.
其中轻稀土亏损的洋中脊型拉斑玄武岩（TH1）的存在显示部分洋壳残片的可能卷入。
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However, relating to investigate the modes, courses and characteristics of the orogenetic process in Paleozoic and after orogenetic process, the cognitive divergence have still occurred.
通过对新疆北东部地区不同构造区带构造作用的方式、过程和特点的研究，确定：①南天山榆树沟高压麻粒岩地体的正变质原岩是一个基本完整的蛇绿岩套，其经历了俯冲至下地壳的高压麻粒岩相、构造抬升至深地壳麻粒岩相以及快速构造折返至角闪岩相的变质过程，代表了南天山洋壳俯冲、变质、随后折返的过程，并首次确定了变质过程的PTt轨迹；②奥陶纪末期中天山北缘发生洋盆俯冲、地体增生作用，此时萨日达拉地区处于岛弧活动带；中石炭世晚期中天山小型洋盆关闭，准噶尔地块与伊犁—中天山板块斜向对接随后发生脆韧性质近水平高温低速右行走滑剪切；③根据巴音沟地区不构成蛇绿岩套有效成分的硅质岩具有与活动大陆边缘密切相关的地球化学特征以及洋中脊玄武岩显示其岩浆源区受到消减带流体交代作用的影响，结合区域地质资料，首次提出巴音沟蛇绿岩带所代表的洋盆古构造环境为弧后盆地，并于早石炭世至中石炭世末期间，经历了扩张、收缩和闭合过程；④首次在克拉麦里蛇绿混杂岩带中分解出具有N-MORB、T-MORB与OIB三种不同类型的火山岩岩石组合，反映了洋盆俯冲
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The mid-oceanic ridge is accreting boundaries. The normal-fault ruptures indicate the tensive stress state in mid-oceanic regions.
大洋中脊是洋壳增生的地区，正断层型的地震破裂显示了洋中脊系的拉张应力状态。
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The difference between MORS- and SSZ-type ophiolites in terms of igneous petrotectonic assemblages is discussed.
探讨了识别洋中脊扩张型和洋俯冲带上面蛇绿岩在火成岩组合上的差别。
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Ridges, also called spreading centers, occur where two plates are moving away from each other.
洋中脊，也叫扩展中心，出现在两个板块相互分离的地方。
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The iron isotopic composition lightly from hydrothermal fluid upwelled into ocean, BIFs are enriched in heavy isotopes of Fe by partial oxidation and precipitation, and iron isotopic composition was homogenous and reequilibrium during different minerals by metamorphism.
提出了地球早期海洋中Fe的循环模式：洋中脊喷发富集Fe轻同位素的二价铁热液流体，流体进入海洋后经过部分氧化和沉淀的过程使得BIF富集Fe的重同位素，后期的变质作用使得不同矿物间发生了Fe的均一化及再平衡
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Three classes of MORBs are distinguished in the transform domain: E-MORBs,Primitive N-MORBs and N-MORBs.Two mantle sources are identified in the Siqueiros region.
转换断层内的洋中脊玄武岩可分三类：富化的洋脊玄武岩、原始的正常洋脊玄武岩(PrimitiveN-MORB)和正常洋脊玄武岩。
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The data show the following ages: 1894±17 Ma and 1847±59 Ma for garnet pyroxenite of the Tiantangshan Group complex, indicating a Paleoproterozoic age; 1462±28 Ma for the metabasic volcanic rocks of the Yunkai Group complex, indicating the presence of fragments of the Meso- and Neoproterozoic oceanic crust in the Yunkai area; 906±24 Ma for the granitic gneiss intrusion is, which should be the product of the global Grenville collisional orogeny occurring around 1000 Ma BP. In addition, an inherited detrital zircon age of 2702±13 Ma was also obtained, which is the oldest age in the Yunkai area and even in Cathaysia, proving the presence of Neoarchean continental crustal material in Cathaysia.
获得天堂山岩群石榴辉石岩的形成年龄为1894Ma±17Ma和1847Ma±59Ma，表明其时代为古元古代；云开岩群洋中脊型变质基性火山岩的喷发年龄为1462Ma±28Ma，证明该地区存在中元古代的古洋壳残片；获得花岗质片麻岩的侵入年龄为906Ma±24Ma，应为1000Ma前后发生的全球性Grenville期造山作用的产物，并获得2702Ma±13Ma的继承碎屑锆石年龄，这是云开地区乃至华夏古陆目前获得的最古老年龄，证明华夏古陆曾存在新太古代陆壳物质。
- 更多网络解释与洋中脊相关的网络解释 [注：此内容来源于网络，仅供参考]
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mid-ocean plateau：洋中海台
mid-ocean canyon 大洋中央峡谷 | mid-ocean plateau 洋中海台 | mid-ocean ridge crest 洋中脊峰线
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mid-ocean canyon：洋中峡谷
中印度洋脊,印度洋中脊 Mid-Indian Ridge | 洋中峡谷 mid-ocean canyon | 洋脊玄武岩 mid-ocean ridge basalt
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mid-ocean rift：大洋中央裂谷,洋中裂谷
洋脊玄武岩 mid-ocean ridge basalt | 大洋中央裂谷,洋中裂谷 mid-ocean rift | 大洋中央裂谷,洋中裂谷 mid-ocean valley
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mid-ocean rise：洋中隆
洋中脊|mid-ocean ridge | 洋中隆|mid-ocean rise | 阳起片岩|actinolite schist
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MOR system：洋中脊系
MOPF 可动油图标志 | MOR system 洋中脊系 | mor 粗腐殖质
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oxygen partial pressure：氧分压
洋中脊玄武岩|mid-ocean ridge basalt | 氧分压|oxygen partial pressure | 氧化膜|oxide film
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pyrolite：地幔岩
岩石圈的厚度究竟有多大,很不一样. 其变化范围从洋中脊地区几乎等于零,到大陆下最深可达 140km. 软流圈则 是根据地震波传播的低速层(LVZ)确定的. 根据这一情况,Ringwood 提出了上地幔的地幔岩(Pyrolite)模型,即
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epicentre：震央
地图揭示出大西洋中央的山脊有着奇怪山谷与山脊的水深测绘(bathymetry),[3]中央山谷的地震活动活跃,同时亦是很多地震的震央(epicentre). [4][5]尤因及希森发现此山脊是一个40000公里长的全球连贯的洋中脊系统的一部分.
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mid-Pacific seamounts：中太平洋海底山群,中太平洋海底山脉
中洋脊,大洋中脊 mid-oceanic ridge | 中太平洋隆起,太平洋中隆 mid-Pacific rise | 中太平洋海底山群,中太平洋海底山脉 mid-Pacific seamounts
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mid-Pacific rise：中太平洋隆起,太平洋中隆
中洋脊,大洋中脊 mid-oceanic ridge | 中太平洋隆起,太平洋中隆 mid-Pacific rise | 中太平洋海底山群,中太平洋海底山脉 mid-Pacific seamounts