首页 > 最新文献

Neues Jahrbuch Fur Mineralogie-Abhandlungen最新文献

英文 中文
Geochemistry, fluid inclusion study and genesis of the sediment-hosted Zn-Pb (± Ag ± Cu) deposits of the Tiran basin, NW of Esfahan, Iran 伊朗伊斯法罕西北部蒂朗盆地沉积型锌铅(±Ag±Cu)矿床地球化学、流体包裹体研究及成因
IF 0.5 4区 地球科学 Q4 Earth and Planetary Sciences Pub Date : 2016-04-01 DOI: 10.1127/NJMA/2016/0301
A. Yarmohammadi, E. Rastad, A. Rajabi
The Tiran basin in the southern part of the Malayer-Esfahan metallogenic belt (MEMB), Iran, contains numerous shalehosted Zn-Pb (± Ag ± Cu) sulfide deposits in black limey siltstone and carbonate rocks of the Early Cretaceous sedimentary sequence. This sequence deposited in an extensional back-arc environment between the Sanandaj-Sirjan Zone (SSZ) and Central Iranian microcontinent. The Tiran Basin consists of six sediment-hosted Zn-Pb deposits (Anjireh-Chekab, Vejin-Bala, Vejin-Paein, Sefidkhal, Khaneh-Sormeh and Kope-Motaleb) with estimated total reserves of 10 Mt at 4 % Zn, 2 % Pb, 0.2 % Cu and 20 ppm Ag. Based on geometry of ores, mineralogy, and texture of sulfide mineralization, three different ore facies can be distinguished in these deposits: feeder zone, massive ore, and extensive banded replacement sulfide ore facies. Silicification, dolomitization and sericitization are the main wall-rock alteration styles; alteration intensity increases toward the feeder zones. The high V/ (V+Ni) values (> 0.6) of the host rocks, and presence of organic matter and framboidal pyrite within fine-grained detrital sediments suggest an anoxic event for the host basin. Fluid inclusions in coarse-grained sphalerite, related to massive and banded replacement ore facies, and hydrothermal calcite, dolomite and quartz that are cogenetic with sulfide minerals in the main stage of mineralization, were studied by microthermometry. Based on fluid inclusion assemblages (FIAs), the homogenization temperatures decrease from the feeder zone (172 °C to 284 °C, av. 205.6 °C) adjacent to the synsedimentary normal faults, through the massive ore (157 °C to 270 °C, av. 195 °C) to the banded replacement ore (115 °C to 270 °C, av. 172 °C) facies. This variation is associated with an increase in salinity from 4.4 through 5.1 to 6.3 wt.% NaCl eq. in the same way. This trend is interpreted to represent mixing of ore fluids with saline seawater at the sub-seafloor unconsolidated sediments in the banded replacement ore facies. Fluid inclusion data show that the Tiran shalehosted Zn-Pb deposits are more like the vent-proximal sedimentary-exhalative (SEDEX) and VMS deposits than other sedimenthosted Zn-Pb deposits, such as Mississippi Valley Type (MVT) and Irish-type mineralizations. However, geological data, ore facies and ore forming processes is compatible with a sub-seafloor replacement SDEDX deposit that has been suggested for some large SEDEX or shale-hosted Zn-Pb deposits such as Red Dog and Anarraaq in Alaska and Century deposit in Australia.
伊朗Tiran盆地位于Malayer-Esfahan成矿带(MEMB)南段,在早白垩世沉积序列的黑色灰质粉砂岩和碳酸盐岩中含有大量泥页岩型Zn-Pb(±Ag±Cu)硫化物矿床。该层序沉积于sanandaji - sirjan带与伊朗中部微大陆之间的伸展弧后环境。Tiran盆地由6个沉积型铅锌矿床(Anjireh-Chekab、Vejin-Bala、Vejin-Paein、Sefidkhal、Khaneh-Sormeh和Kope-Motaleb)组成,估计总储量为1000万吨,含4% Zn、2% Pb、0.2% Cu和20ppm Ag。根据矿石的几何形状、矿物学特征和硫化物矿化结构特征,可将矿床划分为三种不同的矿相:给矿带、块状矿相和广泛的带状替代硫化物矿相。硅化、白云化和绢云母化是主要的围岩蚀变类型;向送料带方向变化强度增大。寄主岩石的高V/ (V+Ni)值(> 0.6),细粒碎屑沉积物中有机质和草莓状黄铁矿的存在表明寄主盆地发生过缺氧事件。用显微测温方法研究了与块状和带状替代矿相有关的粗粒闪锌矿和与硫化物矿物同生的热液方解石、白云石和石英中的流体包裹体。基于流体包裹体组合(FIAs),均一温度从靠近同沉积正断层的给矿带(172°C ~ 284°C,相对205.6°C),通过块状矿石(157°C ~ 270°C,相对195°C)到带状替代矿石(115°C ~ 270°C,相对172°C)逐渐降低。这种变化与盐度从4.4到5.1到6.3 wt.% NaCl当量以同样的方式增加有关。这一趋势被解释为在带状替代矿相的海底松散沉积物中,矿流体与咸水混合。流体包裹体数据表明,与密西西比河谷型(MVT)和爱尔兰型(Irish-type)矿化相比,Tiran页岩含锌铅矿更接近于喷口-近端沉积-喷发型(SEDEX)和VMS矿床。然而,地质数据、矿相和成矿过程与海底替代SDEDX矿床相一致,该矿床已被建议用于一些大型SEDEX或页岩型锌铅矿床,如阿拉斯加的Red Dog和Anarraaq以及澳大利亚的Century矿床。
{"title":"Geochemistry, fluid inclusion study and genesis of the sediment-hosted Zn-Pb (± Ag ± Cu) deposits of the Tiran basin, NW of Esfahan, Iran","authors":"A. Yarmohammadi, E. Rastad, A. Rajabi","doi":"10.1127/NJMA/2016/0301","DOIUrl":"https://doi.org/10.1127/NJMA/2016/0301","url":null,"abstract":"The Tiran basin in the southern part of the Malayer-Esfahan metallogenic belt (MEMB), Iran, contains numerous shalehosted Zn-Pb (± Ag ± Cu) sulfide deposits in black limey siltstone and carbonate rocks of the Early Cretaceous sedimentary sequence. This sequence deposited in an extensional back-arc environment between the Sanandaj-Sirjan Zone (SSZ) and Central Iranian microcontinent. The Tiran Basin consists of six sediment-hosted Zn-Pb deposits (Anjireh-Chekab, Vejin-Bala, Vejin-Paein, Sefidkhal, Khaneh-Sormeh and Kope-Motaleb) with estimated total reserves of 10 Mt at 4 % Zn, 2 % Pb, 0.2 % Cu and 20 ppm Ag. Based on geometry of ores, mineralogy, and texture of sulfide mineralization, three different ore facies can be distinguished in these deposits: feeder zone, massive ore, and extensive banded replacement sulfide ore facies. Silicification, dolomitization and sericitization are the main wall-rock alteration styles; alteration intensity increases toward the feeder zones. The high V/ (V+Ni) values (> 0.6) of the host rocks, and presence of organic matter and framboidal pyrite within fine-grained detrital sediments suggest an anoxic event for the host basin. Fluid inclusions in coarse-grained sphalerite, related to massive and banded replacement ore facies, and hydrothermal calcite, dolomite and quartz that are cogenetic with sulfide minerals in the main stage of mineralization, were studied by microthermometry. Based on fluid inclusion assemblages (FIAs), the homogenization temperatures decrease from the feeder zone (172 °C to 284 °C, av. 205.6 °C) adjacent to the synsedimentary normal faults, through the massive ore (157 °C to 270 °C, av. 195 °C) to the banded replacement ore (115 °C to 270 °C, av. 172 °C) facies. This variation is associated with an increase in salinity from 4.4 through 5.1 to 6.3 wt.% NaCl eq. in the same way. This trend is interpreted to represent mixing of ore fluids with saline seawater at the sub-seafloor unconsolidated sediments in the banded replacement ore facies. Fluid inclusion data show that the Tiran shalehosted Zn-Pb deposits are more like the vent-proximal sedimentary-exhalative (SEDEX) and VMS deposits than other sedimenthosted Zn-Pb deposits, such as Mississippi Valley Type (MVT) and Irish-type mineralizations. However, geological data, ore facies and ore forming processes is compatible with a sub-seafloor replacement SDEDX deposit that has been suggested for some large SEDEX or shale-hosted Zn-Pb deposits such as Red Dog and Anarraaq in Alaska and Century deposit in Australia.","PeriodicalId":51139,"journal":{"name":"Neues Jahrbuch Fur Mineralogie-Abhandlungen","volume":null,"pages":null},"PeriodicalIF":0.5,"publicationDate":"2016-04-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"76353007","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 13
Crystal chemistry of a Ni-Mg analogue of lyonsite from slags of Lavrion, Greece 希腊Lavrion渣中镍镁类似物的晶体化学研究
IF 0.5 4区 地球科学 Q4 Earth and Planetary Sciences Pub Date : 2016-04-01 DOI: 10.1127/NJMA/2016/0297
N. Koshlyakova, N. Zubkova, I. Pekov, G. Giester, D. Pushcharovsky, N. Chukanov, P. Voudouris, A. Magganas, A. Katerinopoulos
{"title":"Crystal chemistry of a Ni-Mg analogue of lyonsite from slags of Lavrion, Greece","authors":"N. Koshlyakova, N. Zubkova, I. Pekov, G. Giester, D. Pushcharovsky, N. Chukanov, P. Voudouris, A. Magganas, A. Katerinopoulos","doi":"10.1127/NJMA/2016/0297","DOIUrl":"https://doi.org/10.1127/NJMA/2016/0297","url":null,"abstract":"","PeriodicalId":51139,"journal":{"name":"Neues Jahrbuch Fur Mineralogie-Abhandlungen","volume":null,"pages":null},"PeriodicalIF":0.5,"publicationDate":"2016-04-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"83061540","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 1
Crystal structure refinement of margarosanite PbCa 2 Si 3 O 9 and relationship with walstromite BaCa 2 Si 3 O 9 辉石pbca2si3o9晶体结构的细化及其与walstromite baca2si3o9的关系
IF 0.5 4区 地球科学 Q4 Earth and Planetary Sciences Pub Date : 2016-04-01 DOI: 10.1127/NJMA/2016/0302
A. Callegari, M. Boiocchi
{"title":"Crystal structure refinement of margarosanite PbCa 2 Si 3 O 9 and relationship with walstromite BaCa 2 Si 3 O 9","authors":"A. Callegari, M. Boiocchi","doi":"10.1127/NJMA/2016/0302","DOIUrl":"https://doi.org/10.1127/NJMA/2016/0302","url":null,"abstract":"","PeriodicalId":51139,"journal":{"name":"Neues Jahrbuch Fur Mineralogie-Abhandlungen","volume":null,"pages":null},"PeriodicalIF":0.5,"publicationDate":"2016-04-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"87142885","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
A new method for the adjustment of Fe2O3/FeO ratio in volcanic rocks for the calculation of CIPW norm 提出了一种调整火山岩中Fe2O3/FeO比值计算CIPW范数的新方法
IF 0.5 4区 地球科学 Q4 Earth and Planetary Sciences Pub Date : 2016-01-01 DOI: 10.1127/njma/2015/0295
E. El-Hinnawi
{"title":"A new method for the adjustment of Fe2O3/FeO ratio in volcanic rocks for the calculation of CIPW norm","authors":"E. El-Hinnawi","doi":"10.1127/njma/2015/0295","DOIUrl":"https://doi.org/10.1127/njma/2015/0295","url":null,"abstract":"","PeriodicalId":51139,"journal":{"name":"Neues Jahrbuch Fur Mineralogie-Abhandlungen","volume":null,"pages":null},"PeriodicalIF":0.5,"publicationDate":"2016-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"85437803","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 3
Imperial porphyry from Gebel Abu Dokhan, the Red Sea Mountains, Egypt.: Part I. Mineralogy, petrology and occurence 来自埃及红海山脉Gebel Abu Dokhan的帝王斑岩。第一部分矿物学、岩石学和产状
IF 0.5 4区 地球科学 Q4 Earth and Planetary Sciences Pub Date : 2016-01-01 DOI: 10.1127/NJMA/2015/0289
E. Makovicky, R. Frei, S. Karup-moller, J. Bailey
{"title":"Imperial porphyry from Gebel Abu Dokhan, the Red Sea Mountains, Egypt.: Part I. Mineralogy, petrology and occurence","authors":"E. Makovicky, R. Frei, S. Karup-moller, J. Bailey","doi":"10.1127/NJMA/2015/0289","DOIUrl":"https://doi.org/10.1127/NJMA/2015/0289","url":null,"abstract":"","PeriodicalId":51139,"journal":{"name":"Neues Jahrbuch Fur Mineralogie-Abhandlungen","volume":null,"pages":null},"PeriodicalIF":0.5,"publicationDate":"2016-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"83811391","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 6
The chemical composition of uranospathite, arsenurano-spathite, and associated minerals revisited: the peculiarity of fluorine incorporation in autunite group minerals 重新探讨了铀磷磷锌矿、砷磷磷磷锌矿及其伴生矿物的化学组成:氟在钙铁矿群矿物中的掺入特性
IF 0.5 4区 地球科学 Q4 Earth and Planetary Sciences Pub Date : 2016-01-01 DOI: 10.15496/PUBLIKATION-17530
G. Markl
{"title":"The chemical composition of uranospathite, arsenurano-spathite, and associated minerals revisited: the peculiarity of fluorine incorporation in autunite group minerals","authors":"G. Markl","doi":"10.15496/PUBLIKATION-17530","DOIUrl":"https://doi.org/10.15496/PUBLIKATION-17530","url":null,"abstract":"","PeriodicalId":51139,"journal":{"name":"Neues Jahrbuch Fur Mineralogie-Abhandlungen","volume":null,"pages":null},"PeriodicalIF":0.5,"publicationDate":"2016-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"73629873","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 1
Geochemistry and petrology of basaltic lavas from NE-Qorveh, Kurdistan province, Western Iran 伊朗西部库尔德斯坦省NE-Qorveh玄武岩熔岩地球化学及岩石学特征
IF 0.5 4区 地球科学 Q4 Earth and Planetary Sciences Pub Date : 2016-01-01 DOI: 10.15496/PUBLIKATION-17559
W. Siebel
{"title":"Geochemistry and petrology of basaltic lavas from NE-Qorveh, Kurdistan province, Western Iran","authors":"W. Siebel","doi":"10.15496/PUBLIKATION-17559","DOIUrl":"https://doi.org/10.15496/PUBLIKATION-17559","url":null,"abstract":"","PeriodicalId":51139,"journal":{"name":"Neues Jahrbuch Fur Mineralogie-Abhandlungen","volume":null,"pages":null},"PeriodicalIF":0.5,"publicationDate":"2016-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"80224546","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 8
Geochemical characteristics of oil shale in the Triassic Chang7 subsection, southern Ordos basin, China, and palaeo-environment reconstruction 鄂尔多斯盆地南部三叠系长7段油页岩地球化学特征及古环境重建
IF 0.5 4区 地球科学 Q4 Earth and Planetary Sciences Pub Date : 2016-01-01 DOI: 10.1127/NJMA/2015/0291
H. Cao, X. Shan, P. Sun, Huanzhao Chi, S. Du
{"title":"Geochemical characteristics of oil shale in the Triassic Chang7 subsection, southern Ordos basin, China, and palaeo-environment reconstruction","authors":"H. Cao, X. Shan, P. Sun, Huanzhao Chi, S. Du","doi":"10.1127/NJMA/2015/0291","DOIUrl":"https://doi.org/10.1127/NJMA/2015/0291","url":null,"abstract":"","PeriodicalId":51139,"journal":{"name":"Neues Jahrbuch Fur Mineralogie-Abhandlungen","volume":null,"pages":null},"PeriodicalIF":0.5,"publicationDate":"2016-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"72697233","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 5
An insight into crystal chemistry and cation order of columbite-(Fe) and columbite-(Mn) from worldwide occurrences 从世界范围内发现的columbit -(Fe)和columbit -(Mn)的晶体化学和阳离子顺序
IF 0.5 4区 地球科学 Q4 Earth and Planetary Sciences Pub Date : 2015-07-01 DOI: 10.1127/NJMA/2015/0285
G. Balassone, R. M. Danisi, T. Armbruster, A. Altomare, A. Moliterni, C. Petti, N. Mondillo, M. Ghiara, M. Saviano
{"title":"An insight into crystal chemistry and cation order of columbite-(Fe) and columbite-(Mn) from worldwide occurrences","authors":"G. Balassone, R. M. Danisi, T. Armbruster, A. Altomare, A. Moliterni, C. Petti, N. Mondillo, M. Ghiara, M. Saviano","doi":"10.1127/NJMA/2015/0285","DOIUrl":"https://doi.org/10.1127/NJMA/2015/0285","url":null,"abstract":"","PeriodicalId":51139,"journal":{"name":"Neues Jahrbuch Fur Mineralogie-Abhandlungen","volume":null,"pages":null},"PeriodicalIF":0.5,"publicationDate":"2015-07-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"73827339","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 3
The jacobsite-magnetite series at the Tumurtijn-ovoo Fe-Mn-Zn skarn deposit, Mongolia 蒙古Tumurtijn-ovoo铁锰锌夕卡岩矿床雅克布长石—磁铁矿系列
IF 0.5 4区 地球科学 Q4 Earth and Planetary Sciences Pub Date : 2015-07-01 DOI: 10.1127/NJMA/2015/0286
W. Gottesmann, B. Gottesmann, W. Seifert, Hans Unger
{"title":"The jacobsite-magnetite series at the Tumurtijn-ovoo Fe-Mn-Zn skarn deposit, Mongolia","authors":"W. Gottesmann, B. Gottesmann, W. Seifert, Hans Unger","doi":"10.1127/NJMA/2015/0286","DOIUrl":"https://doi.org/10.1127/NJMA/2015/0286","url":null,"abstract":"","PeriodicalId":51139,"journal":{"name":"Neues Jahrbuch Fur Mineralogie-Abhandlungen","volume":null,"pages":null},"PeriodicalIF":0.5,"publicationDate":"2015-07-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"78381423","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 1
期刊
Neues Jahrbuch Fur Mineralogie-Abhandlungen
全部 Acc. Chem. Res. ACS Applied Bio Materials ACS Appl. Electron. Mater. ACS Appl. Energy Mater. ACS Appl. Mater. Interfaces ACS Appl. Nano Mater. ACS Appl. Polym. Mater. ACS BIOMATER-SCI ENG ACS Catal. ACS Cent. Sci. ACS Chem. Biol. ACS Chemical Health & Safety ACS Chem. Neurosci. ACS Comb. Sci. ACS Earth Space Chem. ACS Energy Lett. ACS Infect. Dis. ACS Macro Lett. ACS Mater. Lett. ACS Med. Chem. Lett. ACS Nano ACS Omega ACS Photonics ACS Sens. ACS Sustainable Chem. Eng. ACS Synth. Biol. Anal. Chem. BIOCHEMISTRY-US Bioconjugate Chem. BIOMACROMOLECULES Chem. Res. Toxicol. Chem. Rev. Chem. Mater. CRYST GROWTH DES ENERG FUEL Environ. Sci. Technol. Environ. Sci. Technol. Lett. Eur. J. Inorg. Chem. IND ENG CHEM RES Inorg. Chem. J. Agric. Food. Chem. J. Chem. Eng. Data J. Chem. Educ. J. Chem. Inf. Model. J. Chem. Theory Comput. J. Med. Chem. J. Nat. Prod. J PROTEOME RES J. Am. Chem. Soc. LANGMUIR MACROMOLECULES Mol. Pharmaceutics Nano Lett. Org. Lett. ORG PROCESS RES DEV ORGANOMETALLICS J. Org. Chem. J. Phys. Chem. J. Phys. Chem. A J. Phys. Chem. B J. Phys. Chem. C J. Phys. Chem. Lett. Analyst Anal. Methods Biomater. Sci. Catal. Sci. Technol. Chem. Commun. Chem. Soc. Rev. CHEM EDUC RES PRACT CRYSTENGCOMM Dalton Trans. Energy Environ. Sci. ENVIRON SCI-NANO ENVIRON SCI-PROC IMP ENVIRON SCI-WAT RES Faraday Discuss. Food Funct. Green Chem. Inorg. Chem. Front. Integr. Biol. J. Anal. At. Spectrom. J. Mater. Chem. A J. Mater. Chem. B J. Mater. Chem. C Lab Chip Mater. Chem. Front. Mater. Horiz. MEDCHEMCOMM Metallomics Mol. Biosyst. Mol. Syst. Des. Eng. Nanoscale Nanoscale Horiz. Nat. Prod. Rep. New J. Chem. Org. Biomol. Chem. Org. Chem. Front. PHOTOCH PHOTOBIO SCI PCCP Polym. Chem.
×
引用
GB/T 7714-2015
复制
MLA
复制
APA
复制
导出至
BibTeX EndNote RefMan NoteFirst NoteExpress
×
0
微信
客服QQ
Book学术公众号 扫码关注我们
反馈
×
意见反馈
请填写您的意见或建议
请填写您的手机或邮箱
×
提示
您的信息不完整,为了账户安全,请先补充。
现在去补充
×
提示
您因"违规操作"
具体请查看互助需知
我知道了
×
提示
现在去查看 取消
×
提示
确定
Book学术官方微信
Book学术文献互助
Book学术文献互助群
群 号:481959085
Book学术
文献互助 智能选刊 最新文献 互助须知 联系我们:info@booksci.cn
Book学术提供免费学术资源搜索服务,方便国内外学者检索中英文文献。致力于提供最便捷和优质的服务体验。
Copyright © 2023 Book学术 All rights reserved.
ghs 京公网安备 11010802042870号 京ICP备2023020795号-1