Xinjiang Petroleum Geology ›› 2023, Vol. 44 ›› Issue (6): 646-656.doi: 10.7657/XJPG20230602
• OIL AND GAS EXPLORATION • Previous Articles Next Articles
ZHANG Changjian(), YANG Debin, LYU Yanping, ZHANG Juan, LI Jie, DING Liming
Received:
2023-03-01
Revised:
2023-08-03
Online:
2023-12-01
Published:
2023-11-29
CLC Number:
ZHANG Changjian, YANG Debin, LYU Yanping, ZHANG Juan, LI Jie, DING Liming. Division and Characteristics of Karst Water System in Early Hercynian Movement in Tahe Oilfield, Tarim Basin[J]. Xinjiang Petroleum Geology, 2023, 44(6): 646-656.
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Table 1.
Classification of hydromorphology of karst in the early Hercynian movement in Tahe oilfield"
岩溶台地 (岩溶水系统) | 古地貌高程/m | 微地貌 | 地表水系 | 地下水系 |
---|---|---|---|---|
Ⅰ号岩溶台地 (高原峡谷水系统) | -300~-100 | 峡谷、峰丛、丘丛和沟谷 | 南北向汇流,对称型树枝状地表水系 | 平面树枝状结构,少量单支状和网状,洞道延伸长度长,个别长达20.0 km,主要为暗河型 |
Ⅱ号岩溶台地 (伏流峡谷水系统) | -350~-300 | 峡谷、溶峰、溶丘和洼地 | 南北向汇流,向斜式树枝状地表水系,主干水系呈深切曲流峡谷、峡谷和伏流-天窗3段结构 | 平面树枝状结构,洞道延伸长度长达8.0 km,主要为伏流型和暗河型 |
Ⅲ号岩溶台地 (深切曲流水系统) | -500~-350 | 曲流峡谷、溶峰、溶丘和洼地 | 东西向汇流,南北向汇流模式的深切曲流地表水系;S94-1地表水系为由北向南的扇形汇流模式 | 平面单支状结构,少量树枝状,延伸长度较短,为0.4~4.0 km,主要为顺河潜流型、伏流型、暗河型、渗流入流型和穿洞型 |
Ⅳ号岩溶台地 (宽谷水系统) | -600~-500 | 溶丘、洼地和平原 | 由北向南汇流,树枝状宽谷地表水系 | 平面单支状结构,洞道延伸长度为0.2~0.4 km,主要为暗河型 |
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