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地质与地球物理研究... [12]
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Bridging soil biogeochemistry and microbial communities (archaea and bacteria) in tropical seagrass meadows
期刊论文
FRONTIERS IN MARINE SCIENCE, 2023, 卷号: 10, 页码: 17
作者:
Nobrega, Gabriel Nuto
;
de Andrade, Pedro Avelino Maia
;
Queiroz, Hermano Melo
;
Pereira, Arthur Prudencio de Araujo
;
Copertino, Margareth da Silva
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浏览/下载:4/0
  |  
提交时间:2023/11/30
coastal wetlands
Ruppia maritima
Halodule wrightii
Fe fractionation
Metabolic pathways
Kerogen-specific isotope variations during the end-Permian mass extinction in South China
期刊论文
EARTH-SCIENCE REVIEWS, 2022, 卷号: 226, 页码: 15
作者:
Jiang, Lei
;
Cai, Chunfang
;
Xiang, Lei
;
Fan, Junxuan
;
Li, Kaikai
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  |  
浏览/下载:19/0
  |  
提交时间:2022/09/02
Kerogen
Pyrite
CAS
delta S-34
delta H-2
delta C-13
End-Permian mass extinction
South China
Taphonomic study of Chuaria fossils from the Ediacaran Lantian biota of South China
期刊论文
PRECAMBRIAN RESEARCH, 2022, 卷号: 369, 页码: 7
作者:
Wang, Wei
;
Guan, Chengguo
;
Zhao, Xianye
;
Fang, Yan
;
Zhou, Chuanming
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  |  
浏览/下载:20/0
  |  
提交时间:2022/07/20
Fossil
Clay minerals
Pyrite
Ediacaran
Taphonomy
Exceptionally preserved hyolithids from the middle Cambrian of North China
期刊论文
GEOLOGICAL MAGAZINE, 2021, 卷号: 158, 期号: 11, 页码: 1951-1959
作者:
Sun, Haijing(孙海静)
;
Sun, Zhixin(孙志新)
;
Zhao, Fangchen(赵方臣)
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  |  
浏览/下载:15/0
  |  
提交时间:2022/01/11
Hyolitha
soft anatomy
taphonomy
epibiont association
Burgess Shale-type Lagerstatte
Deep-water dissolved iron cycling and reservoir size across the Ediacaran-Cambrian transition
期刊论文
CHEMICAL GEOLOGY, 2020, 卷号: 541, 页码: 9
作者:
Xiang, Lei
;
Schoepfer, Shane D.
;
Zhang, Hua
;
Chen, Zhen-wu
;
Cao, Chang-qun
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  |  
浏览/下载:14/0
  |  
提交时间:2020/10/28
Hetang Formation
Iron isotope
Oceanic dissolved iron reservoir
Oceanic iron cycle
Cambrian explosion
Magnetic mineral diagenesis in sediments of saline lake Lop Nur
期刊论文
JOURNAL OF MOUNTAIN SCIENCE, 2019, 卷号: 16, 期号: 3, 页码: 548-560
作者:
Li Wen
;
Mu Gui-jin
;
Lin Yong-chong
;
Song Hao-ze
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  |  
浏览/下载:21/0
  |  
提交时间:2020/11/02
Early diagenesis
Magnetic properties
Saline lake
Lop Nur
Geological characteristics, formation age and high-grade ore genesis of Zankan banded iron deposit in the West Kunlun Mountains
期刊论文
ACTA PETROLOGICA SINICA, 2018, 卷号: 34, 期号: 2, 页码: 427-446
作者:
Li ZhiQuan
;
Zhang LianChang
;
Xue ChunJi
;
Zheng MengTian
;
Zhu MingTian
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  |  
浏览/下载:33/0
  |  
提交时间:2018/09/29
Sedimentary-metamorphic Iron Deposit
Hydrothermal Modification
Zircon U-pb Age
West Kunlun
Zankan Iron Deposit
High-grade Iron Ore Genesis
Fluid inclusions and stable isotopes study of Shuanghe Au deposit in western Henan
期刊论文
ACTA PETROLOGICA SINICA, 2018, 卷号: 34, 期号: 12, 页码: 3539-3552
作者:
Gao Shuai
;
Zeng QingDong
;
Chu ShaoXiong
;
Zhou TianCheng
;
Fan HongRui
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  |  
浏览/下载:48/0
  |  
提交时间:2019/03/21
Fluid inclusions
Stable isotopes
Shuanghe Au deposit
Southern margin of North China Craton
烟台夹河口外柱状沉积物还原性无机硫、活性铁的变化特征及其相互关系
期刊论文
海洋科学, 2018, 卷号: 42, 期号: 8, 页码: 90-97
作者:
姜明
;
赵国强
;
李兆冉
;
盛彦清
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  |  
浏览/下载:20/0
  |  
提交时间:2020/07/08
还原性无机硫
活性铁
深层柱状沉积物
硫化度
矿化度
Reduced inorganic sulfur
Reactive iron
Deep core sediments
Degree of pyritization
Degree of sulfidity
The distribution characteristics and coupling mechanism of reduced inorganic sulfur (RIS)and reactive iron in marine core sediments are closely related to the evolution of environment quality.In this study,an improved cold diffusion method and hydrochloric acid extraction method were applied to the acid-volatile sulfur (AVS),pyrite sulfur (CRS),elemental sulfur (ES),and reactive iron [Fe (Ⅱ)and Fe (III)] analyses.The distribution characteristics and coupling mechanism of S and Fe were investigated based on a core sediment 4 meters deep collected in the northern sea area of the mouth of Jiahe River,Yantai.The results showed that the RIS in sediments was dominated by CRS,followed by AVS and ES.The content of AVS presented a narrow range with depth,whereas the CRS and ES were higher at the top and bottom layers than the middle layer
reactive iron was dominated by Fe (II),which increased with depth,while Fe (Ⅲ)gradually decreased with depth.Most of the Fe (III)was reduced to the disssolved Fe(II),which was combined with the soluble H_2S of the sulfate-reducing bacteria to produce CRS and ES in the deep layer,resulting in their accumulation at the bottom of core sediments.Furthermore,this study showed that reactive iron was not a limiting factor for the accumulation of RIS with lower degree of pyritization and degree of sulfidity.
Early diagenetic greigite as an indicator of paleosalinity changes in the middle Miocene Paratethys Sea of central Europe
期刊论文
GEOCHEMISTRY GEOPHYSICS GEOSYSTEMS, 2017, 卷号: 18, 期号: 7, 页码: 2634-2645
作者:
Liu, Suzhen
;
Krijgsman, Wout
;
Dekkers, Mark J.
;
Palcu, Dan
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浏览/下载:15/0
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提交时间:2017/11/24
Paratethys
greigite
Miocene
salinity
eccentricity
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