圖版說(shuō)明

圖版說(shuō)明

圖版Ⅰ Plate Ⅰ

a-泰山彩石溪 27.5億年斜長(zhǎng)角閃巖被 27億年英云閃長(zhǎng)巖侵入,二者在26億年被奧長(zhǎng)花崗巖脈侵入;

b-蒙山龜蒙頂25.4億年片麻狀花崗閃長(zhǎng)巖形成的象形石;

c-沂源魯山由25.2億年的二長(zhǎng)花崗巖組成;

d-沂源魯山南側(cè)的溶洞-江北最美石花洞;

e-嶧山丹丸峰;

f-棗莊店子包體帶;

g-臨朐沂山獅子崮由25億年的二長(zhǎng)花崗巖組成;

h-長(zhǎng)島百丈崖蓬萊群輔子夼組石英巖夾千枚巖

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

圖版II Plate II

a-青州云門(mén)山奧陶紀(jì)馬家溝群灰?guī)r;

b-棗莊熊耳山張夏組灰?guī)r遭受 300年前郯城大地震影響形成崩塌遺跡;

c-新泰寺山三山子組疊層石白云巖;

d-威海劉公島位于蘇魯造山帶東段, 由 7～8億年的變質(zhì)變形花崗巖組成, 含有大量的榴輝巖包體;

e-昆崳山九龍池瀑布沿著1.5億年的二長(zhǎng)花崗巖裂隙沖刷;

f-五蓮縣九仙山1.2億年二長(zhǎng)花崗巖形成的峰林地貌;

g-棲霞艾山海蝕作用形成的海豚象形石;

h-日照河山海蝕遺跡

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

圖版III Plate III

a-乳山岠隅山頂?shù)暮Ｎg遺跡;

b-即墨市馬山石林由柱狀節(jié)理發(fā)育的潛英安巖組成;

c-莒南中生代砂巖中恐龍足跡及波痕構(gòu)造;

d-諸城白堊紀(jì)王氏群紅土崖組的恐龍化石;

e-萊陽(yáng)白堊紀(jì)王氏群紅土崖組的恐龍化石;

f-昌樂(lè)火山口被柱狀玄武巖充填;

g-臨朐山旺古生物化石產(chǎn)于解家河盆地臨朐群山旺組地層中; h-郯城麥坡300年前的郯城大地震遺跡

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