郝家河砂岩型铜矿床产于滇中中生代陆相红色碎屑岩建造中，规模中型。
The Haojiahe sandstone copper deposit occurs in the red elastic rock formation of Mesozoic continental facies in central Yunnan, being a medium size one.
准噶尔盆地南缘的郝家沟剖面三叠系—侏罗系连续发育，是研究三叠系—侏罗系界线及相关地质问题的重要剖面。
The Haojiagou section, located in the southern margin of the Junggar Basin, is of great significance in studying the Triassic-Jurassic Boundary events.
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