本书系统研究了萨彦-图瓦高地的地形演化过程，核心内容包括：\n第四纪冰川作用：划分晚更新世（阿扎斯冰期）、中更新世（卡热姆冰期）和早更新世（奇维冰期）三次冰期，分析冰盖范围与消退机制。\n火山活动：研究克鲁泡特金火山、佩列波利奇火山等年轻火山群，揭示玄武岩熔岩流与冰川的相互作用。\n新构造运动：探讨断裂带对地形重塑的影响，如叶尼塞河与安加拉河流域的水系重组。\n应用价值：为南西伯利亚矿产开发（石棉、石墨、金等）与水电工程（安加拉-叶尼塞梯级电站）提供地质依据。\n
", "ds_source": "作者（编委会）：М. Г. 格罗斯瓦利（М. Г. Гросвальд）\n出版社：Издательство «Наука» \n出版地：莫斯科\n出版年：1965年\n页数：166页\n语种：俄文\n分类号：УДК 551.4(571.52)\n馆藏条形码：XJLASRU70000707\n
", "ds_process_way": "本书为中国科学院新疆生态与地理研究所文献信息中心（以下简称中心）馆藏文献，中心将本书电子化后存储，已完成OCR识别，数据加工过程依据国家标准《GB/T 31219.2-2014图书馆馆藏资源数字化加工规范》，完全遵照《萨彦-图瓦高地地形发育》的数据信息，未改动删减。\n
", "ds_quality": "对收集到的《萨彦-图瓦高地地形发育》进行电子化加工处理，按照国家标准《GB/T 31219.2-2014图书馆馆藏资源数字化加工规范》要求，未改动删减《萨彦-图瓦高地地形发育》的数据信息，数据质量可靠。\n
", "ds_acq_start_time": "2025-06-01 00:00:00", "ds_acq_end_time": "2025-06-01 00:00:00", "ds_acq_place": "中亚", "ds_acq_lon_east": null, "ds_acq_lat_south": null, "ds_acq_lon_west": null, "ds_acq_lat_north": null, "ds_acq_alt_low": null, "ds_acq_alt_high": null, "ds_share_type": "login-access", "ds_total_size": 40990949, "ds_files_count": 1, "ds_format": "PDF格式", "ds_space_res": "无", "ds_time_res": "无", "ds_coordinate": "无", "ds_projection": "无", "ds_thumbnail": "42a8c341-7fd7-4f62-accf-89dc716b36af.png", "ds_thumb_from": 0, "ds_ref_way": "", "paper_ref_way": "", "ds_ref_instruction": "", "ds_from_station": null, "organization_id": "a5877b42-96ea-4f13-af7e-246f355413d6", "doi_value": "", "subject_codes": [ "170.45" ], "quality_level": 1, "publish_time": "2025-07-30 10:47:08", "first_publish_time": null, "last_updated": "2026-04-24 11:40:24", "protected": false, "protected_to": null, "lang": "zh", "cstr": "33110.11.ariddc.01101", "license": null, "extra": null, "files_shape": [ { "name": "20250601101(XJLASRU70000707).pdf", "size": 40990949, "is_dir": false } ], "features": null, "data_level": 0, "i18n": { "en": { "title": "Terrain development in the Sayan-Tuva Highlands", "ds_abstract": "This book systematically studies the terrain evolution process of the Sayan-Tuva Highlands. The core contents include:\nQuaternary glaciation: Divide three ice ages: the Late Pleistocene (Azas Glacial Age), the Middle Pleistocene (Kajem Glacial Age) and the Early Pleistocene (Qiwi Glacial Age), and analyze the extent and retreat mechanism of the ice sheet.\nVolcanic activity: Study young volcanic groups such as the Kropotkin Volcano and Peljepolic Volcano to reveal the interaction between basalt lava flows and glaciers.\nNeotectonic movement: Explore the impact of fault zones on terrain reshaping, such as the reorganization of water systems in the Yenisei and Angara River basins.\nApplication value: Provide geological basis for mineral development (asbestos, graphite, gold, etc.) and hydropower projects (Angara-Yenisei Cascade Hydropower Station) in South Siberia.\n
", "ds_source": "Author (Editorial Board): Mr.Г. Groswali (Mus.Г.Гросвальд）\nPublished by: 丨 зда тельство « 丨 аука» \nPublished: Moscow\nPublication year: 1965\nPages: 166 pages\nLanguage: Russian\nClassification No.: У п б 551.4(571.52)\nCollection barcode: XJLASRU70000707\n
", "ds_process_way": "This book is the collection of the Documentation and Information Center of the Xinjiang Institute of Ecology and Geography, China Academy of Sciences (hereinafter referred to as the Center). The center has stored the book electronically and completed OCR recognition. The data processing process is in accordance with the national standard \"GB/T 31219.2-2014 Specifications for Digital Processing of Library Collection Resources\", and fully complies with the data information of \"Terrain Development of the Sayan-Tuva Highlands\" without modification or deletion.\n
", "ds_quality": "The collected \"Topographical Development of Sayan-Tuva Highlands\" was electronically processed. In accordance with the requirements of the national standard \"GB/T 31219.2-2014 Code for Digital Processing of Library Collection Resources\",\"Sayan-Tuva Highlands\" was unchanged and deleted. The data information of \"Topographical Development of Sayan-Tuva Highlands\" is reliable.\n
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