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发表于 2025-3-21 17:57:25
书目名称Mantle and Lower Crust Exposed in Oceanic Ridges and in Ophiolites影响因子(影响力)<br> http://figure.impactfactor.cn/if/?ISSN=BK0623446<br><br> <br><br>书目名称Mantle and Lower Crust Exposed in Oceanic Ridges and in Ophiolites影响因子(影响力)学科排名<br> http://figure.impactfactor.cn/ifr/?ISSN=BK0623446<br><br> <br><br>书目名称Mantle and Lower Crust Exposed in Oceanic Ridges and in Ophiolites网络公开度<br> http://figure.impactfactor.cn/at/?ISSN=BK0623446<br><br> <br><br>书目名称Mantle and Lower Crust Exposed in Oceanic Ridges and in Ophiolites网络公开度学科排名<br> http://figure.impactfactor.cn/atr/?ISSN=BK0623446<br><br> <br><br>书目名称Mantle and Lower Crust Exposed in Oceanic Ridges and in Ophiolites被引频次<br> http://figure.impactfactor.cn/tc/?ISSN=BK0623446<br><br> <br><br>书目名称Mantle and Lower Crust Exposed in Oceanic Ridges and in Ophiolites被引频次学科排名<br> http://figure.impactfactor.cn/tcr/?ISSN=BK0623446<br><br> <br><br>书目名称Mantle and Lower Crust Exposed in Oceanic Ridges and in Ophiolites年度引用<br> http://figure.impactfactor.cn/ii/?ISSN=BK0623446<br><br> <br><br>书目名称Mantle and Lower Crust Exposed in Oceanic Ridges and in Ophiolites年度引用学科排名<br> http://figure.impactfactor.cn/iir/?ISSN=BK0623446<br><br> <br><br>书目名称Mantle and Lower Crust Exposed in Oceanic Ridges and in Ophiolites读者反馈<br> http://figure.impactfactor.cn/5y/?ISSN=BK0623446<br><br> <br><br>书目名称Mantle and Lower Crust Exposed in Oceanic Ridges and in Ophiolites读者反馈学科排名<br> http://figure.impactfactor.cn/5yr/?ISSN=BK0623446<br><br> <br><br>
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发表于 2025-3-21 22:10:56
An Ultramafic Lift at the Mid-Atlantic Ridge: Successive Stages of Magmatism in Serpentinized Peridoalong the Mid-Atlantic Ridge to constrain a model for the building of the lower crust at magma-starved ocean ridges. This model involves successive stages of magmatism within mantle rocks that are rising up from the asthenosphere, and throughout the axial lithosphere, to ultimately form seafloor exp
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发表于 2025-3-22 02:40:40
Gabbroic Dikelets in Serpentinized Peridotites from the Mid-Atlantic Ridge at 23°20’Nes show evidence of minor magmatic intrusion that produced millimetre to centimetre thick gabbroic dikelets. The nature of the intruding magma and the time relationships between intrusion events and tectonic evolution of the host peridotites is inferred from the mineralogy and textural features of v
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发表于 2025-3-22 05:54:04
Mafic and Ultramafic Intrusions into Upper Mantle Peridotites from Fast Spreading Centers of the Eased by the R.V. Sonne. One of these areas is located on the western boundary of the microplate along the West Rift zone near 24°13′S and 115°41′W, and is associated with a small transform fault called Terevaka. The other area consists of a depression called the Pito Deep located at the northern tip o
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发表于 2025-3-22 10:09:27
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发表于 2025-3-22 13:38:50
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发表于 2025-3-22 18:42:27
A Detailed Study of Mantle Flow away from Diapirs in the Oman Ophioliteop of mantle diapirs. In the Oman ophiolite, however, the shear direction inversion is not systematically developed at the same level in the ophiolite sequence. In particular, in the vicinity of mantle diapirs, the uppermost mantle forced flow diverging from the diapir has a clear outward (top away
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发表于 2025-3-22 22:02:33
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发表于 2025-3-23 09:14:35
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