• Title deed/registration document obtained at most three (3) months before the application date or a document that will replace these documents (Notarized)
• Signature circular of the owners mentioned in this document, if the owners do not apply, their notarized consent/power of attorney
• Sample map samples of the parcel or parcels marked for the proposal
• Proposal plan sheet prepared by the author or author organizations that will undertake the preparation of the zoning plans on the plans/current maps in force and endorsed by the relevant professional chamber
• Plan Explanation Report containing the Reviews and Researches prepared in the quality and content stipulated in the Regulation on the Principles of Plan Preparation
• Chamber of Urban Planners office registration document.
  
  

Detailed information can be obtained from geology, geophysics, civil engineers' chambers, universities and building inspection companies.

Techniques for Calculating Earthquake Magnitude

ML (Richter Scale): It was developed by Charles Richter in 1930 and is defined as the logarithm of the wave amplitude. All other scales were developed based on the Richter scale.
Ml: is calculated according to Richter's original relation. It is used for shallow, nearby and small earthquakes (Local magnitude).
Mb: It is calculated based on the amplitude of P and S waves (Body-wave magnitude).
Mb = log10(A/T) + Q(D,h)
Here;
A : Amplitude of grain vibrations (ground motion) (micron);
T: Period (second);
Q(D,h) correction factor, function of the distance between the epicenter and the recorder (D -degrees) and the focal depth (h -kilometer).
Md :It is calculated using the duration of very small and nearby earthquakes (Duration magnitude).
MS :It is calculated based on the amplitude of surface waves (Surface-wave magnitude).
MS = log10 (A/T) + 1.66 log10 (D) + 3.30
Mw :From the seismic moment of the released energy (Moment magnitude).
Seismic moment; is a measure of the magnitude of the earthquake-producing source and is calculated as follows;
Mo=mAu
Here m is the resistance of the rocks to shear stress, A is the broken (i.e. sliding) section of the fault level, and u is the average displacement, i.e. slip, that occurs along the fault. A very important point here is that there is a relationship between u and the fault length. The higher the u, the longer the fault should be.
The moment magnitude is calculated using the following formula:
Mw = 2/3 log10(MO) – 10.7
Me :The amount of energy released by the earthquake, the measure of the damage potential in structures (Here, the energy unit is erg.)
Me =2/3 log10E-9.9
For every 1 unit increase in magnitude, the amount of seismic energy increases approximately 32 times.
After any earthquake, different values ​​are given for the magnitude of the earthquake and differences between countries or institutions are generally due to the different calculation techniques mentioned above.