Application of the non-seismic geophysical method in the deep geological structure study of Benxi-Huanren area

Geodesic radar method is a non-destructive geophysical method to detect underground geological structure based on the differences in conductivity, magnetism and dielectric constants of different substances. This method has the advantages of economy, fast, continuous, accurate, non-destructive, non-contact, etc. It is applicable to both metal and non-metal pipelines, and it is the preferred tool for underground pipeline detection. In this paper, the geological radar method is used to detect the complex pipe network around Daning Reservoir in detail by laying out multiple detection lines. It provides basic support for the later pipe network rectification. The research results can provide experience for the detection of the complex pipe network in the urban reservoir.

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Assembly of VP26 in herpes simplex virus-1 capsid implicated by 3-D structure of recombinant capsid

Proceedings, annual meeting, Electron Microscopy Society of America ◽

10.1017/s0424820100140579 ◽

1995 ◽

Vol 53 ◽

pp. 840-841

Author(s):

Z. Hong Zhou ◽

Jing He ◽

Joanita Jakana ◽

J. D. Tatman ◽

Frazer J. Rixon ◽

...

Keyword(s):

Herpes Simplex Virus ◽

Herpes Simplex ◽

3D Structure ◽

Structure Study ◽

Herpes Simplex Virus 1 ◽

Shell Proteins ◽

Life Threatening ◽

Infected Cells ◽

Simplex Virus ◽

Hsv 1

Herpes simplex virus-1 (HSV-1) is a ubiquitous virus which is implicated in diseases ranging from self-curing cold sores to life-threatening infections. The 2500 Å diameter herpes virion is composed of a glycoprotein spike containing, lipid envelope, enclosing a protein layer (the tegument) in which is embedded the capsid (which contains the dsDNA genome). The B-, and A- and C-capsids, representing different morphogenetic stages in HSV-1 infected cells, are composed of 7, and 5 structural proteins respectively. The three capsid types are organized in similar T=16 icosahedral shells with 12 pentons, 150 hexons, and 320 connecting triplexes. Our previous 3D structure study at 26 Å revealed domain features of all these structural components and suggested probable locations for the outer shell proteins, VP5, VP26, VP19c and VP23. VP5 makes up most of both pentons and hexons. VP26 appeared to bind to the VP5 subunit in hexon but not to that in penton.

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The geological structure of the Emilia-Tuscany Northern Apennines and Alpi Apuane

Geological Field Trips ◽

10.3301/gft.2019.07 ◽

2019 ◽

Vol 11 (2.5) ◽

pp. 1-78 ◽

Cited By ~ 1

Author(s):

Paolo Conti ◽

Gianluca Cornamusini ◽

Luigi Carmignani ◽

Giancarlo Molli

Keyword(s):

Geological Structure ◽

Northern Apennines

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FEATURES OF GEOLOGICAL STRUCTURE AND PETROLEUM OIL POTENTIAL OF VICHULOVSKAYA FORMATION WITHIN VOSTOCHNO-KAMENNYI DEPOSIT (WESTERN SIBERIA)

Moscow University Bulletin. Series 4. Geology ◽

10.33623/0579-9406-2018-2-33-39 ◽

2018 ◽

pp. 33-39

Author(s):

R. R. Gabdullin ◽

O. N. Biryukova ◽

R. A. Akhmedov

Keyword(s):

Western Siberia ◽

Geological Structure ◽

Test Results ◽

Geological Information ◽

Petroleum Oil

The analysis of geological and geophysical materials in order to study the peculiarities of the geological structure of the Vikulov Formation within the Vodorazdel license area was carried out. The presented factual material makes it possible to characterize the geological structure of the investigated area more informatively and for interpreting of seismic materials. The analysis of geological information (GIS and test results) confirms the approved water–oil contact (WOC) level in the investigated section of the deposit, which makes it possible to recalculate its reserves.

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