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[期刊论文] 作者:Dwijesh RAY,Ranadip BANERJEE,S, 来源:地质学报:英文版 年份:2009
从北中央印度山脉(NCIR ) 检验的暗岩的玻璃和矿物质化学在二个变换差错的附近附近提供卓见进岩浆开始:Vityaz (vt ) 和 Vema (VM ) 。从外部山脉胁腹( vt 区域)和一座近山脉...
[期刊论文] 作者:Dwijesh RAY,Ranadip BANERJEE,S, 来源:地质学报:英文版 年份:2008
摘要:来自里面的 Serpentinites 角落高度(6??...
[期刊论文] 作者:Dwijesh RAY,Ranadip BANERJEE,S, 来源:黑龙江科技学院学报 年份:2009
为探究吕家坨井田地质构造格局,根据钻孔勘探资料,采用分形理论和趋势面分析方法,研究了井田7...
[期刊论文] 作者:Dwijesh RAY,Ranadip BANERJEE,Sridhar D.IYER,Subir MUKHOPADHYAY, 来源:地质学报(英文版) 年份:2008
Serpentinites from the inside cer high (6°38.5’S/ 68°19.34’E) from the North Central Indian Ridge (NCIR) are comprised mainly of high Mg-rich lizardite and...
[期刊论文] 作者:Dwijesh RAY,Ranadip BANERJEE,Sridhar D.IYER,Subir MUKHOPADHYAY,, 来源:Acta Geologica Sinica(English Edition) 年份:2008
Serpentinites from the inside corner high(6°38.5′S/68°19.34′E)from the Northern Central Indian Ridge(NCIR)are comprised mainly of high Mg-rich lizardite and...
[期刊论文] 作者:Dwijesh RAY,Sridhar D. IYER,Ranadip BANERJEE,Saumitra MISRA,M. WIDDOWSON,, 来源:Acta Geologica Sinica(English Edition) 年份:2007
Mid-Ocean Ridge Basalts (MORB) from the Northern Central Indian Ridge (NCIR) were recovered between latitudes 3° and 11° S and are olivine tholeiite with high...
[期刊论文] 作者:Mahima Singh,Jayant Singhal,K.Arun Prasad,V.J.Rajesh,Dwijesh Ray,Priyadarshi Sahoo,, 来源:Geoscience Frontiers 年份:2016
Banded iron formations(BIFs) are major rock units having hematite layers intermittent with silica rich layers and formed by sedimentary processes during late Ar...
[期刊论文] 作者:Dwijesh RAY,Ranadip BANERJEE,Sridhar D IYER,Basavaraju BASAVALINGU,Subir MUKHOPADHYAY4,, 来源:Acta Geologica Sinica(English Edition) 年份:2009
The glass and mineral chemistry of basalts examined from the northern central Indian ridge (NCIR) provides an insight into magma genesis around the vicinity of...
[期刊论文] 作者:Mahima Singh,Jayant Singhal,K.Arun Prasad,V.J.Rajesh,Dwijesh Ray,Priyadarshi Sahoo,, 来源:Geoscience Frontiers 年份:2016
Banded iron formations(BIFs) are major rock units having hematite layers intermittent with silica rich layers and formed by sedimentary processes during late Archean to mid Proterozoic time. In terres...
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