浅粒岩

粗面岩、响岩、粗玄岩，含钾泥灰岩、钾长浅粒岩等尚待开发利用。

The trachyte , phonolite , dolerite , K-bearing marl , K-feldspar leptite etc are to be exploited and utilized .

分布在大别造山带南部的浅变质岩层，主要岩石类型为粉砂质千枚岩、变层纹状硅质板岩、变火山角砾岩及浅粒岩，原岩是火山&碎屑沉积岩系。

Epimetamorphic rock series distributed in the south of the Dabie Orogenic Belt are a sequence of volcanic clastic rock series , mainly composed of silty phyllite , laminated siliceous slate , meta volcanic breccia and leptite .

斜长角闪岩-浅粒岩为同一岩浆连续分异变质火山岩，锆石Pb严重丢失，207Pb/206Pb年龄≥（2488±8）Ma。

Amphibolite-leptite is meta-volcanic rocks resulting from continuous differentiation of the same magma . Zircon Pb loss is serious and the 207Pb / 206Pb age is ≥ 2488 ± 8 Ma .

深熔效应以小觉地区的夕线石钾长浅粒岩最为典型。

The effect of the anatexis is most prominent in sillimanite-K-feldspar leucogranulitite ( leptite ) of the Xiaojue area .

花岗质岩石与其围岩变（浅）粒岩为渐变过渡关系，并呈现一些特殊的结构构造。

The granite , which is transitional to its host rock granulite , possesses some special structure and texture , fluctuating largely in its chemical component concentration .