Seismological and Structural Evolution of North Anatolian Fault Zone in the Sea of  Marmara (16pt Times New Roman, Bold, Centered)

STUDENT NAMES (Capital, 12pt Times New Roman, centered)
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Abstract: - This is a sample of the format of your full paper. A concise summary of your paper is given. Entices the reader to want to read on; makes the reader curious about the details contained in the rest of your paper.  Use Word for Windows (Microsoft) (or equivalent Word Processor with exactly the same "printing results") by tuning -1.3 cm from right and -1.3 cm from left in the Microsoft Word package, or equivalently by keeping 1.8 cm, real distance, from right and 1.8 cm, real distance, from left. Use single space. Use double-column format after the Key-Words. Use 11pt, Times New Roman. For the words Abstract, Key-Words and References use Italics.

Key-Words: - Leave one blank line after the Abstract and write your Key-Words (6 - 10 words)

1   Introduction
As you can see for the title of the paper you must use 16pt, Centered, Bold, Times New Roman. Leave one blank line and then type AUTHORS' NAMES (in Capital, 12pt Times New Roman, centered), Department (in 12pt Times New Roman, centered), University (in 12pt Times New Roman, centered), Address (in 12pt Times New Roman, centered), COUNTRY (in Capital, 12pt Times New Roman, centered). Then you must type your e-mail address  youremailaccount@xxx.xxx.xx and your Web Site address http://www.yourwebaddress.xxx.xx (both in 12pt Times New Roman, centered). 
     The heading of each section should be printed in small, 14pt, left justified, bold, Times New Roman. You must use numbers 1, 2, 3, … for the sections' numbering and not Latin numbering (I, II, III, …) Introduces geography and tectonic setting of the region to the reader. Defines the objective of your paper (“to understand the crustal structure and tectonic evolution of….”  Summarizes how you went about achieving your objective (“research constrains on crustal structure and tectonic evolution offered by geophysical observations” States specific geophysical studies reported on in the literature. Offers conclusions, perhaps in the form of general models (or competing models), that can be developed from those studies.

2   Observations and Interpretations
Please, leave two blank lines between successive sections as here. 
     Mathematical Equations must be numbered as follows: (1), (2), …, (99) and not (1.1), (1.2),…, (2.1), (2.2),… depending on your various Sections.

2.1	Seismic Refraction
Potential constrains now available; Overall crustal thickness; Pattern of crustal thickness changes; Internal crustal velocities; Uppermost mantle velocities; Potential newobservations and interpretations: Thin crust at a continental rift or mid ocean ridge?; Thick crust at a mountain range?; Transition from thick continental to thin oceanic crust at a continental margin? Low upper-mantle velocities at a continental margin? Low upper-mantle velocities at a continental rift or mid-ocean ridge? When including a subsection you must use, for its heading, small letters, 12pt, left justified, bold, Times New Roman as here. 

2.1.1   Sub-subsection 
When including a sub-subsection you must use, for its heading, small letters, 11pt, left justified, bold, Times New Roman as here.

2.2	Sismic Reflection 
Same as like Seismic Refraction.

2.2.1   Sub-subsection 
When including a sub-subsection you must use, for its heading, small letters, 11pt, left justified, bold, Times New Roman as here.

2.3	Earthquake 
Potential constrains now available; Positions of lithospheric plate boundaries; Types of stresses in the region; Lithospheric thickness changes based on seismic delay times Potential new observations and interpretations: Shallow earthquakes at divergent and transform boundaries? Earthquakes to considerable depth at convergent boundaries? Normal fault focal plane solutions showing areas of extension? Reverse fault focal plane solutions showing areas of compression? Strike-slip fault focal plane solutions showing areas of shearing stress? Thin lithosphere at a continental rift or mid-ocean ridge? Thick lithosphere at a subduction zone or collisional mountain range?

3   Discussion
Presents your own discussion on how the constrains contribute to understanding the crustal structure and tectonic evolution of the regions.

Figures and Tables should be numbered as follows: Fig.1, Fig.2, … etc Table 1, Table 2, ….etc.
     If your paper deviates significantly from these specifications, our Publishing House may not be able to include your paper in the Proceedings. When citing references in the text of the abstract, type the corresponding number in square brackets as shown at the end of this sentence [1]. 

4   Conclusion
Sates what you conclude from your synthesis/analysis.

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References:
[1] X1. Author, Title of the Paper, International Journal of Science and Technology, Vol.X, No.X, 19XX, pp. XX-XX.
[2] X2. Author, Title of the Book, Publishing House, 19XX