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| 1 | Plkl: unexpected roles in DNA replication显示文摘 | Ranadip Mandal Klaus Strebhardt | 2013 | Cell Research2013，23，11： | 2 |
| 2 | Glass and Mineral Chemistry of Northern Central Indian Ridge Basalts:Compositional Diversity and Petrogenetic Significance显示文摘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 two transform faults: Vityaz (VT) and Vema (VM). The studied mid-ocean ridge basalts (MORBs) from the outer ridge flank (VT area) and a near-ridge seamount (VM area) reveal that they are moderately phyric plagioclase basalts composed of plagioclase (phenocryst [An60-90] and groundmass [An35-79]), olivine (Fo81-88), diopside (Wo45-51, En25-37, Fs14-24), and titanomagnetite (FeOt~63.75 wt% and TiO2~22.69 wt%). The whole-rock composition of these basalts has similar Mg# [mole Mg/mole(Mg+Fe2+)] (VT basalt:~0.56-0.58; VM basalt:~0.57), but differ in their total alkali content (VT basalt:~2.65; VM basalt:~3.24). The bulk composition of the magma was gradually depleted in MgO and enriched in FeOt, TiO2, P2O5, and Na2O with progressive fractionation, the basalts were gradually enriched in Y and Zr and depleted in Ni and Cr. In addition, the ΣREE of magma also increased with fractionation, without any change in the (La/ Yb)N value. Glass from the VM seamount shows more fractionated characters (Mg#: 0.56-0.57) compared to the outer ridge flank lava of the VT area (Mg#: 0.63-0.65). This study concludes that present basalts experienced low-pressure crystallization at a relatively shallow depth. The geochemical changes in the NCIR magmas resulted from fractional crystallization at a shallow depth. As a consequence, spinel was the first mineral to crystallize at a pressure >10 kbar, followed by Fe-rich olivine at <10 kbar pressure. | Dwijesh RAY Ranadip BANERJEE Sridhar D IYER Basavaraju BASAVALINGU Subir MUKHOPADHYAY4 | 2009 | Acta Geologica Sinica(English Edition)2009，83，6： | 2 |
| 3 | A New Report of Serpentinites from Northern Central Indian Ridge(at 6°S)—An Implication for Hydrothermal Activity显示文摘摘要:来自里面的 Serpentinites 角落高度(6?? | Dwijesh RAY Ranadip BANERJEE Sridhar D.IYER Subir MUKHOPADHYAY | 2008 | Acta Geologica Sinica(English Edition)2008，82，6： | 1 |
| 4 | 显示文摘 | M. Guptha Ranadip Banerjee Lina Mergulhao | 2002 | Geo - Marine Letters2002，，1： | 1 |
| 5 | Ligand stimulation of CD95 induces activation of PIk3 followed by phosphorylation of caspase-8显示文摘在有它的 ligand 的 CD95 受体的相互作用之上,适配器分子 FADD (MORT1 ) 的顺序的协会, caspases-8/10,和 caspase-8/10 管理者 c 扭动支持形式导致导致死亡的发信号建筑群的形成。这里,我们识别像马球的 kinase (Plk ) 3 死亡受体 CD95 作为一个新相互作用合伙。Plk3 的酶的活动与它的 ligand 增加 CD95 受体的后面的相互作用。大美人(击倒) 或 caspase-8, CD95 或 FADD 击倒在 CD95 刺激之上阻止 Plk3 的激活,为 Plk3 激活建议一个功能的磁盘的一个要求。而且,我们为 Plk3 作为新底层识别 caspase-8。Phosphorylation 在 T273 上发生并且导致 caspase-8 proapoptotic 功能的刺激。在在一个营救实验或在 CRISPR/Cas9 产生的 Plk3 击倒房间表示 non-phosphorylatable caspase-8-T273A 异种的房间的 CD95 的刺激减少显著地处理 caspase-8。低 T273 phosphorylation 在 95 个肛门肿瘤病人的一个队与低 Plk3 表示显著地相关。我们的数据在 Plk 家庭以内建议 kinase 激活的新奇机制并且与高 Plk3 在肿瘤为外来的死亡小径的刺激建议一个新模型表示。 | Christina Helmke Monika Raab Franz Rodel Yves Matthess Thomas Oellerich Ranadip Mandal Mourad Sanhaji Henning Urlaub Claus Rodel Sven Becker Klaus Strebhardt | 2016 | Cell Research2016，26，8： | 1 |
| 6 | Mineralogical and geochemical variation in hydrothermal sulfides from Vienna Woods field,Manus Basin,Papua New Guinea:constraints on their evolution显示文摘Polymetallic sulfides from two hydrothermal chimneys and talus deposit from the Vienna Woods field of Manus Basin were studied for mineralogy,elemental composition,and S-isotope ratio to understand their evolution.The factors including the nature of source fluid,mineral paragenesis,and related geochemical processes have been discussed.Mineralogy and elemental concentration of Cu and Fe-rich large chimney at the central part of this hydrothermal field was completely different from the smaller Zn-rich peripheral chimney and Fe-rich talus deposit,suggesting the variable degree of alterations generate physico-chemically different source fluids responsible for these hydrothermal structures.Similarly,S-isotope ratios also indicate chemically diverse fluids and different modes of precipitation were involved in their evolution.Distinct mineral zonings and associated elemental and isotopic compositions within individual deposit confirm paragenetic shifts were involved during their growth process. | RAY Durbar BANERJEE Ranadip MAZUMDER Aninda PAROPKARI Anil L. MUKHOPADHYAY Subir BALAKRISHNAN Srinivasan | 2018 | Acta Oceanologica Sinica2018，37，4： | 1 |
| 7 | A Petrogenetic Model of Basalts from the Northern Central Indian Ridge:3-11°S显示文摘 | Dwijesh RAY Sridhar D. IYER Ranadip BANERJEE Saumitra MISRA M. WIDDOWSON | 2007 | Acta Geologica Sinica(English Edition)2007，81，1： | 0 |
| 8 | Early Pliocene Paleoceanography of the Vityaz Fracture Zone,Central Indian Ridge显示文摘从铁锰合金脚听的石灰质的底层的 Planktic 有孔虫类 Vityaz 断裂带(VFZ ) ,中央印度理兹被学习重建这个区域的早上新世苍白的海洋学。planktic 有孔虫类的十一种被遇到,在他们之中 Globorotalia menardii, Neogloboquadrina dutertrei, Globigerina bulloides andGlobigerinoides ruber 是突出的。N 的优势。在顶的 dutertrei 3 厘米碳酸盐底层被归因于最后由增加滋养的水平触发了他们的生产率的淡水的流入。G 的存在。bulloides 和 G。在在更深的层的重要比例的 menardii 在 welling 上面建议开的海洋的流行。在不同深度间隔的底层的体积化学成分在能被在上新世的山峰期间陆上的物质捱过的化学药品通过海洋的水供应了的上面的节显示踪迹金属的更高的丰富亚洲季风。因此,在早上新世期间,底层的源於生物的部件被两个清楚地在 welling 上面贡献,生产率由淡水在早上新世时期期间从亚洲季风的增强发源的流入被触发,这被结束。 | M.V.S.GUPTHA Ranadip BANERJEE Lina P.MERGULHAO Priyanka BANERJEE G.PARTHIBAN Manish TEWARI | 2007 | Acta Geologica Sinica(English Edition)2007，81，4： | 0 |
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