A. Миколайчук1, Ф. Апаяров1,2, Д. Гордеев1, А. Эсминцев3
1Кыргызский институт минерального сырья, Бишкек, Кыргызстан
2Институт геологии НАН, Бишкек, Кыргызстан
3Институт геологических наук, Алматы, Казахстан
Миколайчук Александр Владимирович,
кандидат геолого-минералогических наук,
720044, Бишкек Кыргызстан, ул. Л. Толстого, 3,
Кыргызский институт минерального сырья,
старший научный сотрудник.
Апаяров Фарид Хурматович,
кандидат геолого-минералогических наук,
720044, Бишкек Кыргызстан, ул. Л. Толстого, 3,
Кыргызский институт минерального сырья,
старший научный сотрудник,
720040, г. Бишкек, бульвар Эркиндик, 30,
Институт геологии им. М.М. Адышева НАН КР,
старший научный сотрудник.
Гордеев Дмитрий Валентинович,
720044, Бишкек Кыргызстан, ул. Л. Толстого, 3,
Кыргызский институт минерального сырья,
инженер.
Эсминцев Александр Николаевич,
050010, Алматы, Казахстан, ул. Валиханова, 69/94,
Институт геологических наук,
старший научный сотрудник.
Аннотация. Исследователями пограничных районов Кыргызстана, Казахстана и Китая активно обсуждают две альтернативные модели соотношения основных структурных единиц Тянь-Шаня. Большинство исследователей считают, что структуры Кыргызского Срединного Тянь-Шаня выклиниваются в восточном направлении вдоль Атбаши-Иныльчек-Налатинского краевого разлома. Согласно второй гипотезе, структуры Срединного Тянь-Шаня продолжаются в пределах хр. Налати, где они описаны как Китайский Центральный Тянь-Шань. Сравнительная характеристика осадочных, вулканогенных, интрузивных и метаморфических формаций палеозоя и протерозоя указанных регионов приводит нас к заключению о том, что структурные единицы Кыргызского Срединного и большей части Северного Тянь-Шаня, включая наложенные средне-позднепалеозойские прогибы, не прослеживаются на территории Китая, а последовательно срезаются вдоль системы кулисно сочленяющихся сдвигов, объединенных нами в Фронтальный Тяньшаньский правый сдвиг (ФТПС). И только северный сегмент Иссыккульского террейна может рассматриваться в качестве аналога китайского Центрального Тянь-Шаня, смещенного вдоль ФТПС к северо-западу на расстояние не менее 80 км. Геологические комплексы срезаются вдоль ФТПС подобно тому, как косые границы сближающихся литосферных плит подвергаются тектонической эрозии.
Ключевые слова: структурное районирование, протерозой, палеозой, U-Pb датировки вулканитов и гранитоидов, Тянь-Шань.
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