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2-amino-4-chloro-3-nitro-benzoic acid | 37901-85-2

中文名称
——
中文别名
——
英文名称
2-amino-4-chloro-3-nitro-benzoic acid
英文别名
2-Amino-4-chlor-3-nitro-benzoesaeure;2-Amino-4-chloro-3-nitrobenzoic acid
2-amino-4-chloro-3-nitro-benzoic acid化学式
CAS
37901-85-2
化学式
C7H5ClN2O4
mdl
——
分子量
216.581
InChiKey
QUELTDJZAOWFCM-UHFFFAOYSA-N
BEILSTEIN
——
EINECS
——
  • 物化性质
  • 计算性质
  • ADMET
  • 安全信息
  • SDS
  • 制备方法与用途
  • 上下游信息
  • 反应信息
  • 文献信息
  • 表征谱图
  • 同类化合物
  • 相关功能分类
  • 相关结构分类

计算性质

  • 辛醇/水分配系数(LogP):
    1.8
  • 重原子数:
    14
  • 可旋转键数:
    1
  • 环数:
    1.0
  • sp3杂化的碳原子比例:
    0.0
  • 拓扑面积:
    109
  • 氢给体数:
    2
  • 氢受体数:
    5

反应信息

  • 作为产物:
    参考文献:
    名称:
    Progress and records in the study of endogenetic mineralization during collisional orogenesis
    摘要:
    To develop and perfect the theory of plate tectonics and regional metallogeny, metallogenesis during collisional orogenesis should be thoroughly studied and wilt attract increasing attention of more and more scientists. This paper presents the main aspects of research and discussions on metallogenesis during collisional orogenesis after the development of plate tectonics, and accordingly divides the study history into two stages, i.e. the junior stage during 1971-1990 and the senior stage after 1990. Beginning with the negation of mineralization in the collision regime by Guild (1971), the focus of study was put on whether there occurred any mineralization during collisional orogenesis at the junior stage. At the senior stage, which is initiated by the advance of metallogenic and petrogenic model for collisional orogenesis, scientists begin to pay their attention to the geodynamic mechanism of metallogenesis, spatial and temporal distribution of ore deposits, ore-forming fluidization, relationship between petrogenesis and mineralization in collisional orogenesis, etc, Abundance of typical collisional orogens such as Himalayan, China has best natural conditions to study collisional metallogenesis. Great progress in the study of metallogenesis during collisional orogenesis has been made by Chinese geologists. Therefore, we hope that the Chinese geologists and Chinese governments at various levels to pay more attention to the study of collisional metallogenesis. Some urgent problems are suggested to be solved so as to bring about breakthroughs in the aspects concerned.
    DOI:
    10.1007/bf02884893
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文献信息

  • US3931303A
    申请人:——
    公开号:US3931303A
    公开(公告)日:1976-01-06
  • US4031074A
    申请人:——
    公开号:US4031074A
    公开(公告)日:1977-06-21
  • Progress and records in the study of endogenetic mineralization during collisional orogenesis
    作者:Yanjing Chen、Huayong Chen、Yulin Liu、Guangjun Guo、Yong Lai、Shan Qin、Baoling Huang、Zengjie Zheng、Yinghui Sui、Chao Li、Zhen Li、Ping Li、Xin Li、Haihua Wang、Meixiang Zhu、Xiuli Gao、Qiying Wei
    DOI:10.1007/bf02884893
    日期:2000.3
    To develop and perfect the theory of plate tectonics and regional metallogeny, metallogenesis during collisional orogenesis should be thoroughly studied and wilt attract increasing attention of more and more scientists. This paper presents the main aspects of research and discussions on metallogenesis during collisional orogenesis after the development of plate tectonics, and accordingly divides the study history into two stages, i.e. the junior stage during 1971-1990 and the senior stage after 1990. Beginning with the negation of mineralization in the collision regime by Guild (1971), the focus of study was put on whether there occurred any mineralization during collisional orogenesis at the junior stage. At the senior stage, which is initiated by the advance of metallogenic and petrogenic model for collisional orogenesis, scientists begin to pay their attention to the geodynamic mechanism of metallogenesis, spatial and temporal distribution of ore deposits, ore-forming fluidization, relationship between petrogenesis and mineralization in collisional orogenesis, etc, Abundance of typical collisional orogens such as Himalayan, China has best natural conditions to study collisional metallogenesis. Great progress in the study of metallogenesis during collisional orogenesis has been made by Chinese geologists. Therefore, we hope that the Chinese geologists and Chinese governments at various levels to pay more attention to the study of collisional metallogenesis. Some urgent problems are suggested to be solved so as to bring about breakthroughs in the aspects concerned.
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