The variolitic andesite from the Susong County in the Dabie Mountains impli
es that it was erupted in water. The mineralogy of the varioles is primaril
y radiate plagioclase (albite sind oligoclase), with little pyroxene, hornb
lende and quartz (derived from alteration). The pyroxene, hornblende and qu
artz are in the interstices between plagiocalse. The matrix consists of gla
ss, hornblende, chlorite, epidote and zoisite. It is clearly subjected an e
xtensive alteration. The andesite has an uncommon chemical composition. The
SiO2 content is about 56.8%, TiO2 = 0.9%, MgO = 6.4%, Fe2O3 (tot) = 6.7%si
milar to 7.6%, 100Mg/(Mg + Fe) = 64.1 similar to 66.2. Mg-# is significantl
y high. The andesite has high abundances of large-lithophile trace elements
(e.g. K, Ba. Sr, LREE), e.g. La/Nb = 5.56 similar to 6.07, low abundances
of high-strength-field elements (HFSE e.g. Ta, Nb, P, Ti), particularly Ta
and Nb strongly depleted. These are consistent with the characteristics of
subduction-related magmas. In the spider diagram of trace elements, from Ce
to right hand, the abundances of elements decrease quickly, showing a char
acter of the continental margins. There has a strong punishment of light-ra
re-earth elements, with a significant diffraction of REEs (the mean value o
f (La/Yb)(N) is 32.84). No Eu anomaly, but there are anomaly high (La/Yb)(N
) = 28.63 similar to 36.74, (La/Y)(N) = 70.33 similar to 82.4. The elements
Y and Yb are depleted greatly, Y<20 <mu>g/g, Y-N = 2.74 similar to 2.84, Y
b-N = 2.18 similar to 2.35. From the La-(La/Sm) diagram, the andesite is de
rived from partial melting. But the epsilone value of Nd is - 18.7 similar
to -19.2, so that the material source may be the mantle materials affected
by the crustal materials. The Nd model age is 1.9 Ga indicating that the va
riolitic basaltic andesite was resulted from the mantle wedge of North Chin
a block, which had the Nd model age of 2.5Ga, when the Yangze block which h
ad the Nd model age of 1.7Ga subducted beneath it. So the variolitic andesi
te has characteristics of the island-are volconic rocks oil a continental b
asement in the vicinity of the destructive continental margin.