king's response seg field camp poster development...king's response seg field camp 2019 eremenko...

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We discovered 2 anomalies corresponding to archaeological sites in the Chinge-tei mound and in the Zhelvak-5 and 2 emptiness on the top of the Chinge-tei mound. This poster presents the key results of SEG Field Camp project called "King's Response", which was performed in the King's Valley, Tyva Republic, Russia. This valley is the greatest archeological site of early Scythian culture. Our project aimed at the investigation the memorial complex Chinge-Tei I and Zhelvak-5. The project was developed and performed by the Students of Novosibirsk State University. The main idea of our project was to research archeological objects by the wide range of geophysical methods and integration different methods on each site. The methods we used are: Magnetometry, Ground Penetrating Radar (GPR), Electrical Tomography (ERT), Electromagnetic Induction Sounding, Passive Seismic. At a depth of 2 meters at around 8 meters from the beginning of the profile, a high-resistance anomaly was found. Maybe this anomaly is associated with the presence of voids. We also conducted investigation by passive seismic on the top of the mound. For the installation of seismic stations, a survey line was selected along which a recording was made for eight observation points with a step of 2 m. The seismic noise spectra of two observation points № 6, 8 contain multiple peaks of standing waves . Spectrum № 8 was calculated for a record lasting 165 minutes (Fig. 3, b). It peaks at frequencies of 100 and 200 Hz. We estimate the depth to the boundary with the void 6.25 m. And on spectrum № 2, the signal duration of which is 95 minutes, frequencies 40, 80, 120 are highlighted, while the depth to the void is 2.5 m . Novosibirsk State University Chapter report of KING'S RESPONSE SEG FIeld Camp 2019 Eremenko Vasiliy, Novosibirsk State University, Russia, [email protected] Belovezhets Nadezhda, Novosibirsk State University, Russia, [email protected] Berezhnev Yaroslav, Novosibirsk State University, Russia, [email protected] Chinge-tei The second site was located at a distance from the main elevation. A reconnaissance magnetic survey was carried out in order to conduct magnetic surveys at 4 levels above the identified anomalies. The dimensions of the studied area are 20 by 16 m. The survey step along the profile is 1 m. The distance from the ground to the lower sensor is about 0.5 m; to the top, 1.5 m. The shooting step between profiles is 1 m. The vertical gradient of the anomalous geomagnetic field during reconnaissance survey at the Chinge-tei mound. The magnetic anomaly circled in an orange circle, green color indicates electrical exploration profiles Magnetic shooting in the search mode revealed a more intense anomaly in the neighboring area, presumably from a ferromagnetic object. As a result, this site was selected for integrating magnetometric and electrometric methods, as well as for interpreting the results of different-height surveys. The size of the plot was 10 by 7 meters. The shooting step along the profile was 0.5 m; the shooting step between the profiles is 1 m. The heights at which the magnetic fields were measured were: 0.30; 0.80; 1.30; 1.80 meters from the ground, respectively. Maps of the module of the anomalous field at the site of the Chinge-tei mound. Orange ovals indicate the position of the obtained magnetic anomalies,, which are signed by numbers 1 and 2. Based on the results of the interpretation of magnetic and electrical exploration: Anomaly 1 - an iron object with magnetic susceptibility about 3000 - 5000 * 10-5 SI at the depth of 0.8-1 m; Anomaly 2 - an archaeological site with magnetic susceptibility about 6.6 - 7.3 * 10-5 SI with the depth of upper edge - 0.5 m, lower - 2.5 m and high resistance . Amplitude spectra of recordings of observation points №8 (a) and 6 (b). The numbers show the peaks corresponding to the nth mode of the standing wave. Zhelvak-5 Archaeological site Chinge-tei is a huge funeral-memorial complex with a diameter of 105 meters. The first site of work was located directly on the southern slope of the mound. The profiles were located from the center of the mound to its periphery with a slight difference in elevation. General view of the monument and the location of the electrotomoghraphy profiles Zhelvak-5 is located at the source of a small nameless log lying in the mountains (southern spurs of the Kurtushibinsky ridge), enclosed between the Zhelvak, Chkalovsky logs and the valley of the drying Zhelvak stream in the Piy-Khem region of the Republic of Tyva. The parking lot is a stretch of land stretched from the northwest to the southeast (the bottom of the log), enclosed between the slopes of the mountains, at the confluence of three drains Topo-plan by Expedition of the Zhogova N.A. At this place a gradient magnetic survey was performed with a step of 1 by 1 meter on a plot measuring 5 by 5 meters. Magnetic variation station was not installed. Since a pit was dug in part of the plot, therefore, the map of the anomalous magnetic field is represented by the cut-out region of the corresponding pit. The height of the sensors from the surface of the earth was 0.5 and 1.5 m, respectively. An abnormal magnetic field at the Zhelvak-5. The orange oval depicts the position of the anomaly of interest (indicated by the number 3). Green color indicates electrical exploration profile On the profiles of electrical exploration (object 2 in Chinge-tei), we observe an extended anomaly with high resistance, which corresponds to the anomaly calculated according to the magnetic exploration data. Using georadar survey, stone placers and sandstones were discovered. Seismic studies were carried out on a straight profile with a step of 2 meters at 4 observation points. The signal accumulation was carried out 110 -140 minutes. The noise accumulation spectra for this object do not contain pronounced peaks of standing waves of multiple frequencies. Based on the results of the interpretation of magnetic and electrical exploration: Most likely object type - Archaeological site with Magnetic susceptibility ~ 7.4 * 10^(-5) SI with the depth of the upper edge - 0.5 m; bottom ~ 3 meters. Special thanks to: Conclusion An example of the spectra of signals from the Zhelvak-5 parking lot that do not have explicit peaks corresponding to standing waves. In total, 5 electrotomography profiles were performed on the Chinge-tei mound with a step of 1 meter between the profiles and 1 meter between the electrodes. The length of each profile using one multi-electrode cable was 24 meters. A high-resistivity region is distinguished in the section, corresponding in outline to a buried burial.

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  • We discovered 2 anomalies corresponding to archaeological sites in theChinge-tei mound and in the Zhelvak-5 and 2 emptiness on the top of theChinge-tei mound.

    This poster presents the key results of SEG Field Camp project called "King'sResponse", which was performed in the King's Valley, Tyva Republic, Russia.This valley is the greatest archeological site of early Scythian culture. Our project aimed at the investigation the memorial complex Chinge-Tei Iand Zhelvak-5. The project was developed and performed by the Students ofNovosibirsk State University. The main idea of our project was to researcharcheological objects by the wide range of geophysical methods and integration different methods on each site. The methods we used are: Magnetometry, Ground Penetrating Radar (GPR),Electrical Tomography (ERT), Electromagnetic Induction Sounding, PassiveSeismic.

    At a depth of 2 meters at around 8 meters from thebeginning of the profile, a high-resistance anomalywas found. Maybe this anomaly is associated with thepresence of voids.

    We also conducted investigation by passive seismic on the top of themound. For the installation of seismic stations, a survey line was selectedalong which a recording was made for eight observation points with a step of 2m. The seismic noise spectra of two observation points № 6, 8 containmultiple peaks of standing waves . Spectrum № 8 was calculated for a recordlasting 165 minutes (Fig. 3, b). It peaks at frequencies of 100 and 200 Hz. Weestimate the depth to the boundary with the void 6.25 m. And on spectrum №2, the signal duration of which is 95 minutes, frequencies 40, 80, 120 arehighlighted, while the depth to the void is 2.5 m .

    Novosibirsk State University Chapter report of

    KING'S RESPONSE SEG FIeld Camp 2019

    Eremenko Vasiliy, Novosibirsk State University, Russia, [email protected] Nadezhda, Novosibirsk State University, Russia, [email protected]

    Berezhnev Yaroslav, Novosibirsk State University, Russia, [email protected]

    Chinge-tei

    The second site was located at a distance from the main elevation. Areconnaissance magnetic survey was carried out in order to conductmagnetic surveys at 4 levels above the identified anomalies. The dimensionsof the studied area are 20 by 16 m. The survey step along the profile is 1 m.The distance from the ground to the lower sensor is about 0.5 m; to the top,1.5 m. The shooting step between profiles is 1 m.

    The vertical gradient of the anomalousgeomagnetic field during reconnaissance

    survey at the Chinge-tei mound. The magneticanomaly circled in an orange circle, green

    color indicates electrical exploration profiles

    Magnetic shooting in the search mode revealed a more intense anomaly inthe neighboring area, presumably from a ferromagnetic object. As a result,this site was selected for integrating magnetometric and electrometricmethods, as well as for interpreting the results of different-height surveys.The size of the plot was 10 by 7 meters. The shooting step along the profilewas 0.5 m; the shooting step between the profiles is 1 m. The heights at whichthe magnetic fields were measured were: 0.30; 0.80; 1.30; 1.80 meters fromthe ground, respectively.

    Maps of the module of the anomalous field atthe site of the Chinge-tei mound. Orange ovals

    indicate the position of the obtainedmagnetic anomalies,, which are signed by

    numbers 1 and 2.

    Based on the results of the interpretation of magnetic and electricalexploration: Anomaly 1 - an iron object with magnetic susceptibility about 3000 - 5000 * 10-5 SI at the depth of 0.8-1 m; Anomaly 2 - an archaeologicalsite with magnetic susceptibility about 6.6 - 7.3 * 10-5 SI with the depth ofupper edge - 0.5 m, lower - 2.5 m and high resistance .

    Amplitude spectra of recordings of observation points №8 (a) and 6 (b). The numbers show the peakscorresponding to the nth mode of the standing wave.

    Zhelvak-5

    Archaeological site Chinge-tei is ahuge funeral-memorial complex with adiameter of 105 meters. The first site ofwork was located directly on thesouthern slope of the mound. Theprofiles were located from the centerof the mound to its periphery with aslight difference in elevation.

    General view of the monument and thelocation of the electrotomoghraphy profiles

    Zhelvak-5 is located at the source ofa small nameless log lying in themountains (southern spurs of theKurtushibinsky ridge), enclosedbetween the Zhelvak, Chkalovsky logsand the valley of the drying Zhelvakstream in the Piy-Khem region of theRepublic of Tyva. The parking lot is astretch of land stretched from thenorthwest to the southeast (thebottom of the log), enclosed betweenthe slopes of the mountains, at theconfluence of three drains

    Topo-plan by Expedition of the Zhogova N.A.

    At this place a gradient magneticsurvey was performed with a step of 1by 1 meter on a plot measuring 5 by 5meters. Magnetic variation station wasnot installed. Since a pit was dug inpart of the plot, therefore, the map ofthe anomalous magnetic field isrepresented by the cut-out region ofthe corresponding pit. The height ofthe sensors from the surface of theearth was 0.5 and 1.5 m, respectively.

    An abnormal magnetic field at the Zhelvak-5. Theorange oval depicts the position of the anomaly ofinterest (indicated by the number 3). Green color

    indicates electrical exploration profile

    On the profiles of electrical exploration (object 2 in Chinge-tei), we observe an extended anomaly with highresistance, which corresponds to the anomaly calculated according to the magnetic exploration data.

    Using georadar survey, stone placers and sandstones were discovered.Seismic studies were carried out on a straight profile with a step of 2 metersat 4 observation points. The signal accumulation was carried out 110 -140minutes. The noise accumulation spectra for this object do not containpronounced peaks of standing waves of multiple frequencies.

    Based on the results of the interpretation of magnetic and electricalexploration: Most likely object type - Archaeological site with Magneticsusceptibility ~ 7.4 * 10^(-5) SI with the depth of the upper edge - 0.5 m;bottom ~ 3 meters.

    Special thanks to:

    Conclusion

    An example of the spectra of signals from the Zhelvak-5 parking lot that do not haveexplicit peaks corresponding to standing waves.

    In total, 5 electrotomography profiles were performed on the Chinge-teimound with a step of 1 meter between the profiles and 1 meter between theelectrodes. The length of each profile using one multi-electrode cable was 24meters. A high-resistivity region is distinguished in the section,corresponding in outline to a buried burial.