Приложение 1 NEOTECTONIC MAP OF SYRIA...

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Neotectonic Map of Syria, 2010 Scale 1:1 000 000 Editors-in-Chief: Dr. Mohamad RUKIEH and Prof. Vladimir G. TRIFONOV Responsible Executor: Prof. Vladimir G. TRIFONOV The map was compiled by: Geological Institute, Russian Academy of Sciences, Moscow, Russia: Dr. Dmitry M. BACHMANOV, Dr. Andrey E. DODONOV, Prof. Vladimir G. TRIFONOV Institute of Dynamics of the Geospheres, Moscow, Russia Tamara P. IVANOVA General Organization of Remote Sensing, Damascus, Syria: Dr. Mohamad RUKIEH, Dr. Osama AMMAR, Dr. Ablul-Majid AL KAFRI, Dr. Haytham MININI, Dr. Mahmoud EBRAHEEM, Tarik ZAZA, Ali YUSEF, Osama ALI, Mohamad ALI Damascus University, Damascus, Syria: Dr. Marwan AL SHARA Organization of Atomic Energy, Damascus, Syria: Dr. Yusef JOBAILI Н еотектоническая карта С ирии, 2010 М асш таб 1:1 000 000 Главны е редакторы : д-р М охам ад РУ К И Е и проф . В.Г. ТРИ ФОНОВ О тветственны й исполнитель: проф . В.Г. ТРИ ФОНОВ К арту составили: Геологический институт Российской академ ии наук, М осква, Россия: д-р Д .М . БАЧМ АН О В , д-р А .Е . Д О ДОНОВ, проф . В.Г. ТРИ ФОНОВ И нститут динам ики геосф ер РАН , М осква , Россия: Т.П . И ВАНОВА Генеральная организация дистанционного зондирования , Д ам аск, С ирия: Д -р М охам ад РУ К И Е , д-р О сам а АМ М АР, д-р А бдул -М адж ид АЛЬ -КАФ РИ , д-р Х ейсам МИНИНИ , д-р М ахм уд Э Б РА Х И М , Т арик ЗА ЗА , А ли Ю ЗЕФ , О сам а А Л И , М охам ад А Л И Д ам асский университет, Д ам аск, С ирия: Д -р М арван А Л Ь-Ш АРА О рганизация атом ной энергии, Д ам аск, С ирия: Д -р Ю зеф Д Ж ОБАЙЛИ р The Map is based on the data of geological mapping in different scales, publications, materials of the General Organization of Remote Sensing of Syria and Syrian Petroleum Company, and results of interpretation of space images and field investigations carried out by the authors. The main used materials are the following: NEOTECTONIC MAP OF SYRIA ( ) Н ЕО ТЕКТО Н И Ч ЕСКАЯ КАРТА СИ РИ И Iskenderon Iskenderon Antakya Antakya Idlib Idlib Mediterranean sea Mediterranean sea Damascus Damascus Beyrouth Beyrouth Lattaqie Lattaqie Banias Banias Hama Hama Tartous Tartous Tripoli Tripoli Homs Homs Haifa Haifa Soweida Soweida Aleppo Aleppo Raqqa Raqqa Euphrates Euphrates Deir ez-zor Deir ez-zor Hassake Hassake Qamichli Qamichli Boukamal Boukamal Palmyra Palmyra 1000 1000 900 900 800 800 700 700 600 600 500 500 500 500 400 400 300 300 200 200 100 100 400 400 800 800 900 900 600 600 700 700 200 200 1000 1000 100 100 300 300 200 200 100 100 1000 1000 100 100 100 100 200 200 200 200 600 600 40 40 60 60 20 20 80 80 60 60 100 100 100 100 100 100 20 20 40 40 1200 1200 300 300 200 200 1000 1000 300 300 800 800 200 200 400 400 200 200 100 100 50 50 10 10 600 600 200 200 300 300 200 200 600 600 400 400 200 200 100 100 100 100 100 100 100 100 50 50 200 200 600 600 600 600 400 400 200 200 100 100 600 600 1200 1200 1000 1000 800 800 400 400 200 200 1800 1800 100 100 300 300 200 200 300 300 800 800 1300 1300 50 50 200 200 400 400 400 400 1000 1000 1000 1000 800 800 600 600 Adiyaman Ö., Chorowicz J. 2002. Late Cenozoic tectonics and volcanism in the northwestern corner of the Arabian plate: a consequence of the strike-slip Dead Sea fault zone and the lateral escape of Anatolia. Jour. of Volcan. Geotherm. Res. 117, No. 3/4, 327–345. Ambraseys N.N., Jackson J.A. 1998. Faulting associated with historical and recent earthquakes in the Eastern Mediterranean. Geophys. Jour. Intern.133, No. 2, 390– 406. Ammar O. 1993. Properties of the geological structure of the South-Western Syria and evaluation of the ground water resources by interpretation of remote sensing data. Ph. D. Thesis, Moscow, 156 p. (In Russian). Barazangi M., Seber D., Chaimov T., Best J., Litak R.D., Sawaf T. 1993. Tectonic evolution of the northern Arabian plate in western Syria. In: Boschi E., Mantovani E., Morelli A. (Eds.) Recent evolution and seismicity of the Mediterranean region. Kluwer Acad. Publ., Dordrecht, 117– 140. Barberi R., Capaldi G., Gasperini P., Marinelli G., Santacroce R., Scandone R., Treuil M., Valet J. 1979. Recent basaltic volcanism of Jordan and its implications on the geodynamic history of the Dead Sea shear zone. Acc. Naz. Lincei, Atti dei Convegni 47, 667– 683. Ben-Avraham Z., Ginzburg A., Markis J., Eppelbaum L. 2002. Crustal structure of the Levant Basin, eastern Mediterranean. Tectonophysics 346, 23–43. Ben-Avraham Z., Hall J.K., Schattner U., Ben-Gai Y., Neev D., Reshef M. 2004. New seismic insights into the tectonic and sedimentary processes in the northeastern Levant. Proc. of the 5th Intern. Sympos. on Eastern Mediterranean Geology, Thessaloniki, 29–31. Ben-Gai Y., Ben-Avraham Z., Buchbinder В ., Kendall C.G.St.C. 2004. Post-Messinian evolution of the Southeastern Levant margin based on stratigraphic modelling. Proc. of the 5th Intern. Sympos. on Eastern Mediterranean Geology, Thessaloniki, 32–34. Brew G., Barazangi M., Al-Maleh K., Sawaf T. 2001. Tectonic Map of Syria, 1:1 000 000. Brew G., Lupa J., Barazangi M., Sawaf T., Al-lmam A., Zaza T. 2001. Structure and tectonic development of the Ghab basin and the Dead Sea fault system, Syria. Jour. Geol. Soc. London 158, 665-674. Brew G., Best J., Barazangi M., Sawaf T. 2003. Tectonic evolution of the NE Palmyride mountain belt, Syria: the Bishri crustal block. Jour. Geol. Soc. London 160, 677– 685. Butler R.W.H., Spenser S., Griffith H.M. 1997. Transcurrent fault activity on the Dead Sea Transform in Lebanon and its implications for plate tectonics and seismic hazard. Jour. Geol. Soc. London 154, 757– 760. Carte Geologique du Liban. 1:250 000 / M.L. Dubertret. 1955. Republique Libanaise, Ministere des Travaux Publics. Chaimov T.A., Barazangi M., Al-Saad D., Sawaf T., Gebran A. 1990. Crustal shortening in the Palmyride fold belt, Syria, and implications for movements along the Dead Sea fault system. Tectonics 9, No. 6, 1369–1386. 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Tectonophysics 357, 255278. 0 100 200 400 35° 36° 37° 38° 39° 40° 41° 42° 43° в.д. 35° 36° 37° 38° 39° 40° 41° 42° 43° в.д. 37° с.д. 36° 35° 34° 33° 32° 37° с.д. 36° 35° 34° 33° 32° 50 50 200 200 200 200 400 400 100 100 К арта основана на данны х геологической съём ки разного м асш таба, публикациях, м атериалов Генеральной организации дистанционного зондирования С ирии и С ирийской неф тяной ком пании, по результатам интерпретации косм ических изображ ений и полевы х исследований авторов. О сновны е использованны е м атериалы : Uplifts, m (П однятия, м ) Isopachs (И зопахиты ) Quaternary sediments Ч етвертичны е отлож ения Pliocene & Quaternary sediments П лиоценовы е и четвертичны е отлож ения Miocene, Pliocene & Quaternary sediments & volcanites М иоценовы е, плиоценовы е и четвертичны е отлож ения и вулканиты Kurd Dagh boundary Граница К урд-Д ага Basins Впадины 600– 1000 1000– 1600 1600– 2000 2000– 2400 > 2400 State boundary Государственная граница Basalts (Б азальты ) Holocene Голоцен Late Pleistocene П оздний плейстоцен Calabrian & Middle Pleistocene К алабрий и средний плейстоцен Pliocene & Gelasian П лиоцен и гелазий Late Miocene (+ Early Pliocene in Shin Plateau) П оздний плиоцен (+ ранний плиоцен на плато Ш ин) Early & Middle Miocene Ранний и средний м иоцен Volcanoes В улканы Lava flows Т ечение лав Volcanic chains Ц епи вулканов Anticlines А нтиклинали Minor, Neogene, unknown sense of motion (proved) М алы е неогеновы е разлом ы с неизвестной кинем атикой (достоверны е ) Faults (Разломы ) Major, Active, Strike-slip (proved) К рупны е активны е сдвиги (достоверны е) Major, Active, Normal (proved) К рупны е активны е сбросы (достоверны е) Major, Active, Normal (supposed) К рупны е активны е сбросы (предполагаем ы е) Major, Active, unknown sense of motion К рупны е активны е разлом ы с неизвестной кинем атикой Minor, Active, Strike-slip (proved) М алы е активны е сдвиги (достоверны е ) Minor, Active, Strike-slip (supposed) М алы е активны е сдвиги (предполагаем ы е ) Minor, Active, Normal (proved) М алы е активны е сбросы (достоверны е ) Minor, Active, Normal (supposed) М алы е активны е сбросы (предполагаем ы е ) Minor, Active, Extension (proved) М алы е активны е раздвиги (достоверны е ) Minor, Active, unknown sense of motion (proved) М алы е активны е разлом ы с неизвестной кинем атикой (достоверны е) Minor, Active, unknown sense of motion (supposed) М алы е активны е разлом ы с неизвестной кинем атикой (предполагаем ы е) Minor, Quaternary, Strike-slip (supposed) М алы е четвертичны е сдвиги (предполагаем ы е) Minor, Quaternary, Thrusts & Reverse (proved) М алы е четвертичны е надвиги и взбросы (достоверны е) Minor, Quaternary, Thrusts & Reverse (supposed) М алы е четвертичны е надвиги и взбросы (предполагаем ы е) Minor, Quaternary, Normal (proved) М алы е четвертичны е сбросы (достоверны е) Minor, Quaternary, Normal (supposed) М алы е четвертичны е сбросы (предполагаем ы е) Minor, Quaternary, Extension (proved) М алы е четвертичны е раздвиги (достоверны е ) Minor, Quaternary, unknown sense of motion (proved) М алы е четвертичны е разлом ы с неизвестной кинем атикой (достоверны е ) Minor,Quaternary,unknownsenseofmotion(supposed) М алы е четвертичны е разлом ы с неизвестнойкинем атикой(предполагаем ы е ) Minor, Neogene, Strike-slip (proved) М алы е неогеновы е сдвиги (достоверны е ) Minor, Neogene, Thrusts & Reverse (proved) М алы е неогеновы е надвиги и взбросы (достоверны е ) Minor, Neogene, Thrusts & Reverse (supposed) М алы е неогеновы е надвиги и взбросы (предполагаем ы е ) Minor, Neogene, Normal (supposed) М алы е неогеновы е сбросы (предполагаем ы е ) Minor, Neogene, Extension (proved) М алы е неогеновы е раздвиги (достоверны е ) Minor, Neogene, Extension (supposed) М алы е неогеновы е раздвиги (предполагаем ы е ) Minor, Neogene, unknown sense of motion ( ) М алы е неогеновы е разлом ы с неизвестной кинем атикой ( ) supposed предполагаем ы е Appendix 1 П рилож ение 1 kilometres

Transcript of Приложение 1 NEOTECTONIC MAP OF SYRIA...

Neotectonic Map of Syria, 2010 Scale 1:1 000 000

Editors-in-Chief: Dr. Mohamad RUKIEH and Prof. Vladimir G. TRIFONOV

Responsible Executor: Prof. Vladimir G. TRIFONOVThe map was compiled by:

Geological Institute, Russian Academy of Sciences, Moscow, Russia:

Dr. Dmitry M. BACHMANOV, Dr. Andrey E. DODONOV, Prof. Vladimir G. TRIFONOV

Institute of Dynamics of the Geospheres, Moscow, RussiaTamara P. IVANOVA

General Organization of Remote Sensing, Damascus, Syria:

Dr. Mohamad RUKIEH, Dr. Osama AMMAR, Dr. Ablul-Majid AL KAFRI, Dr. Haytham MININI,

Dr. Mahmoud EBRAHEEM, Tarik ZAZA, Ali YUSEF, Osama ALI, Mohamad ALI

Damascus University, Damascus, Syria:Dr. Marwan AL SHARA

Organization of Atomic Energy, Damascus, Syria: Dr. Yusef JOBAILI

Н еотектоническая карта Сирии, 2010М асш таб 1:1 000 000

Главные редакторы : д-р М охамад РУК И Е и проф . В.Г. ТРИ Ф О Н О В

О тветственный исполнитель: проф . В.Г. ТРИ Ф О Н О В

К арту составили:Геологический институт Российской академии наук,

М осква, Россия: д-р Д .М . БАЧМ АН О В, д-р А.Е. ДО ДО Н О В,

проф . В.Г. ТРИ Ф О Н О ВИ нститут динамики геосфер РАН , М осква, Россия:

Т.П . И ВАН О ВАГенеральная организация дистанционного зондирования,

Дамаск, Сирия:Д-р М охамад РУК И Е, д-р О сама АМ М АР,

д-р Абдул-М аджид АЛЬ-К АФ РИ , д-р Хейсам М И Н И Н И , д-р М ахмуд ЭБРАХИ М , Тарик ЗАЗА, Али Ю ЗЕФ , О сама АЛИ ,

М охамад АЛИДамасский университет, Дамаск, Сирия:

Д-р М арван АЛЬ-Ш АРАО рганизация атомной энергии, Дамаск, Сирия:

Д-р Ю зеф ДЖ О БАЙ ЛИ

р

The Map is based on the data of geological mapping in different scales, publications, materials of the General

Organization of Remote Sensing of Syria and Syrian Petroleum Company,

and results of interpretation of space images and field investigations carried out by the authors.

The main used materials are the following:

NEOTECTONIC MAP OF SYRIA ( )Н ЕО ТЕКТО Н И ЧЕСКАЯ КАРТА СИ РИ И

IskenderonIskenderon

AntakyaAntakya

IdlibIdlib

Mediterranean sea

Mediterranean sea

DamascusDamascus

BeyrouthBeyrouth

LattaqieLattaqie

BaniasBanias

HamaHama

TartousTartous

TripoliTripoli

HomsHoms

HaifaHaifa

SoweidaSoweida

AleppoAleppo

RaqqaRaqqa

EuphratesEuphrates

Deir ez-zorDeir ez-zor

HassakeHassake

QamichliQamichli

BoukamalBoukamal

PalmyraPalmyra

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0 100 200 400

35° 36° 37° 38° 39° 40° 41° 42° 43° в.д.

35° 36° 37° 38° 39° 40° 41° 42° 43° в.д.

37°

с.д.

36°

35°

34°

33°

32°

37°

с.д.

36°

35°

34°

33°

32°

5050

200

200

200

200

400

400

100

100

К арта основана на данных геологической съёмки разного масш таба, публикациях, материалов Генеральной

организации дистанционного зондирования Сирии и Сирийской нефтяной компании,

по результатам интерпретации космических изображений и полевых исследований авторов.

О сновные использованные материалы :

Uplifts, m (П однятия, м)

Isopachs (И зопахиты )Quaternary sedimentsЧетвертичные отложенияPliocene & Quaternary sedimentsП лиоценовые и четвертичные отложенияMiocene, Pliocene & Quaternary sediments & volcanitesМ иоценовые, плиоценовые и четвертичные отложения и вулканитыKurd Dagh boundaryГраница К урд-Дага

BasinsВпадины

600–1000

1000–1600

1600–2000

2000–2400

> 2400

State boundaryГосударственная граница

Basalts (Базальты)HoloceneГолоценLate PleistoceneП оздний плейстоценCalabrian & Middle PleistoceneК алабрий и средний плейстоценPliocene & GelasianП лиоцен и гелазийLate Miocene (+ Early Pliocene in Shin Plateau)П оздний плиоцен (+ ранний плиоцен на плато Ш ин)Early & Middle Miocene Ранний и средний миоцен

VolcanoesВулканыLava flowsТечение лавVolcanic chainsЦ епи вулкановAnticlinesАнтиклинали

Minor, Neogene, unknown sense of motion (proved)М алые неогеновые разломы с неизвестной кинематикой (достоверные)

Faults (Разломы)

Major, Active, Strike-slip (proved)К рупные активные сдвиги (достоверные)Major, Active, Normal (proved)К рупные активные сбросы (достоверные)

Major, Active, Normal (supposed)К рупные активные сбросы (предполагаемые)

Major, Active, unknown sense of motionК рупные активные разломы с неизвестной кинематикой

Minor, Active, Strike-slip (proved)М алые активные сдвиги (достоверные)

Minor, Active, Strike-slip (supposed)М алые активные сдвиги (предполагаемые)

Minor, Active, Normal (proved)М алые активные сбросы (достоверные)Minor, Active, Normal (supposed)М алые активные сбросы (предполагаемые)

Minor, Active, Extension (proved)М алые активные раздвиги (достоверные)

Minor, Active, unknown sense of motion (proved)М алые активные разломы с неизвестной кинематикой (достоверные)Minor, Active, unknown sense of motion (supposed)М алые активные разломы с неизвестной кинематикой (предполагаемые)

Minor, Quaternary, Strike-slip (supposed)М алые четвертичные сдвиги (предполагаемые)Minor, Quaternary, Thrusts & Reverse (proved)М алые четвертичные надвиги и взбросы (достоверные)

Minor, Quaternary, Thrusts & Reverse (supposed)М алые четвертичные надвиги и взбросы (предполагаемые)Minor, Quaternary, Normal (proved)М алые четвертичные сбросы (достоверные)Minor, Quaternary, Normal (supposed)М алые четвертичные сбросы (предполагаемые)

Minor, Quaternary, Extension (proved)М алые четвертичные раздвиги (достоверные)Minor, Quaternary, unknown sense of motion (proved)М алые четвертичные разломы с неизвестной кинематикой (достоверные)Minor, Quaternary, unknown sense of motion (supposed)М алые четвертичные разломы с неизвестной кинематикой (предполагаемые)

Minor, Neogene, Strike-slip (proved)М алые неогеновые сдвиги (достоверные)Minor, Neogene, Thrusts & Reverse (proved)М алые неогеновые надвиги и взбросы (достоверные)

Minor, Neogene, Thrusts & Reverse (supposed)М алые неогеновые надвиги и взбросы (предполагаемые)Minor, Neogene, Normal (supposed)М алые неогеновые сбросы (предполагаемые)Minor, Neogene, Extension (proved)М алые неогеновые раздвиги (достоверные)Minor, Neogene, Extension (supposed)М алые неогеновые раздвиги (предполагаемые)

Minor, Neogene, unknown sense of motion ( )М алые неогеновые разломы с неизвестной кинематикой ( )

supposedпредполагаемые

Appendix 1П риложение 1

kilometres