图版说明

图版说明

图版Ⅰ Plate Ⅰ

a-泰山彩石溪 27.5亿年斜长角闪岩被 27亿年英云闪长岩侵入,二者在26亿年被奥长花岗岩脉侵入;

b-蒙山龟蒙顶25.4亿年片麻状花岗闪长岩形成的象形石;

c-沂源鲁山由25.2亿年的二长花岗岩组成;

d-沂源鲁山南侧的溶洞-江北最美石花洞;

e-峄山丹丸峰;

f-枣庄店子包体带;

g-临朐沂山狮子崮由25亿年的二长花岗岩组成;

h-长岛百丈崖蓬莱群辅子夼组石英岩夹千枚岩

a-rocks showing 2.75 Ga amphibolite intruded by 2.7 Ga tonalite, and both of them intruded by 2.6 Ga trondhjemite, Colorful Stone Stream of Taishan;

b-hieroglyphic stone composed of 2.54 Ga gneissic granodiorite, Guimengding of Mengshan;

c-2.52 Ga monzogranite, Lushan, Yiyuan;

d-Shihua cave, south of Lushan, Yiyuan;

e-Danwan peak, Yishan;

f-enclave belt, Dianzi, Zaozhuang;

g-stone lion composed of 2.5 Ga monzogranite, Yishang, Linqu;

h-quartzite and phyllite interlayers of the Fuzikuang Formation of the Penglai Group, Changdao Baizhangya

图版II Plate II

a-青州云门山奥陶纪马家沟群灰岩;

b-枣庄熊耳山张夏组灰岩遭受 300年前郯城大地震影响形成崩塌遗迹;

c-新泰寺山三山子组叠层石白云岩;

d-威海刘公岛位于苏鲁造山带东段, 由 7～8亿年的变质变形花岗岩组成, 含有大量的榴辉岩包体;

e-昆嵛山九龙池瀑布沿着1.5亿年的二长花岗岩裂隙冲刷;

f-五莲县九仙山1.2亿年二长花岗岩形成的峰林地貌;

g-栖霞艾山海蚀作用形成的海豚象形石;

h-日照河山海蚀遗迹

a-limestone of the Ordovician Majiagou Group, Yunmenshan, Qingzhou;

b-limestone of the Zhangxia Formation which suffered Tancheng earthquake 300 years ago, and hence generated landslip relics of Xionger Mountain, Zaozhuang;

c-stromatolite dolomite of the Sanshanzi Formation, Sishan, Xiantai;

d-Liugongdao, located in the east of Su-Lu orogeny, is composed of 700-800 Ma deformed granite with many eclogite enclaves;

e-Jiulongchi Falls of Kunyushan flowing along the fracture of 150 Ma monzogranite;

f-peak-forest landform composed of 120 Ma monzogranite, Jiuxianshan, Wulian;

g-dolphin hieroglyphic stone generated by sea erosion, Aishan, Qixia;

h-sea erosion relics, Heshan, Rizhao

图版III Plate III

a-乳山岠隅山顶的海蚀遗迹;

b-即墨市马山石林由柱状节理发育的潜英安岩组成;

c-莒南中生代砂岩中恐龙足迹及波痕构造;

d-诸城白垩纪王氏群红土崖组的恐龙化石;

e-莱阳白垩纪王氏群红土崖组的恐龙化石;

f-昌乐火山口被柱状玄武岩充填;

g-临朐山旺古生物化石产于解家河盆地临朐群山旺组地层中; h-郯城麦坡300年前的郯城大地震遗迹

a-sea erosion relics, top of Juyushan, Rushan;

b-Mashan stone forests composed of dacite with abundant columnar jointings, Jimo City;

c-dinosaur footprints and ripple structures in the Mesozoic sandstone, Junan;

d-dinosaur fossils of the Cretaceous Hongtuya Formation of the Wangshi Group, Zhucheng;

e-dinosaur fossils of the Cretaceous Hongtuya Formation of the Wangshi Group, Laiyang;

f-a volcanic vent filled with columnar basalt, Changle;

g-Shanwang palaeobios fossils occurring in the Shanwang Formation of the Linqu Group, Linqu;

h-Tancheng earthquake relics formed 300 years ago, Maipo, Tancheng