Abstracts of Acta Geologica Sinica (Chinese Edition) Vol. 79,No. 3,2005

Geochemical Characteristics of Fossil Ginkgo huttonii Cuticles from the Jurassic in Gansu, China，Diatoms of Lacustrine Sediments and Paleo-environments in Dahyab Tso (Taicuo) Lake, Xi‘zang (Tibet)，^40Ar/^39Ar Dating for the Strike-slip Movement on the Feidong Part of the Tanlu Fault Zone，Tectonic Origin of Klippen at the Foot of the Wuliangshan Thrust Belt, Western Yunnan……     

Abstracts of Acta Geologica Sinica （Chinese Edition） Vol. 80, No. 3, 2006

Differential Salt Tectonic Deformation and Segmentation of the Kuqa Foreland Fold-Thrust Belt, Tarim Basin, Northwest China TANG Liangjie, LI Jingchang, YU Yixin, WANG Qinghua, YANG Wenjing, XIE Huiwen, CHEN Shuping and PENG Gengxin (Key Laboratory for Hydrocarbon Accumulation, China University of Petroleum, Ministry of Education, Beijing 102249; Basin & Reservoir Research Center, China University of Petroleum, Beijing 102249; Department of Earth Resources Engineering, Kyushu University, Japan; 4. Tarim Oilfield Company, PetroChina Company Ltd., Korla, Xinjiang 841000; 5.     

Abstracts of Acta Geologica Sinica (Chinese Edition) Vol. 74, No. 3, 2000

The paper reports SHRIMP U-Pb zircon data of a dark-coloured eclogite and a post-eclogite garnet-bearing gneissic-granitic rock from the Bixiling area, Yuexi County, Anhui Province, in the eastern Dabie Mountains. The eclogite, which is metamorphosed basic tuff, contains very scarce zircons in omphacite or garnet, but more in quartz. They usually exhibit a     

Abstracts of Acta Geologica Sinica (Chinese Edition) Vol. 78, No. 3,2004

A Taxanomic Study on Primitive EuconodontsWU Guichun, YAO Jianxin and JI Zhansheng(Institute of Geology, Chinese Academy of Geological Sciences,Beijing 100037)Primitive euconodonts are extrmely abundant and varied in the Late Cambrian in western Shandong Province. Two new genera are established, including Camconodontus gen. nov. and Laiwunodus gen. nov. Among them the following species are described: Camconodontus rotundatus gen. et sp. nov., Camconodontus sp., Laiwunodus lateronodus gen. et sp. nov., and     

Johillerit,Na(Mg,Zn)3 Cu(AsO4)3, ein neues Mineral aus Tsumeb,Namibia

Zusammenfassung Die chemische Analyse des neuen Minerals Johillerit mit der Elektronenmikrosonde ergab: Na₂O 5,4, MgO 18,3, ZnO 5,4, CuO 15,8 und As₂O₅ 55,8, Summe 100.7%. Aus diesem Ergebnis wurde die idealisierte Formel Na(Mg, Zn)₃ Cu(AsO₄)₃ abgeleitet. Johillerit ist monoklin mit der RaumgruppeC2/c. Die Gitterkonstanten sind:a=11,870 (3),b=12,755 (3),c=6,770 (2) , =113,42 (2)°,Z=4. Die stärksten Linien des Pulverdiagramms sind: 4,06 (5) (22 ), 3,50 (4) (310), 3,25 (8) (11 ), 2,75 (10) (330, 240), 2,64 (5) (311, 13 , 40 ), 1,952 (4) (13 , 35 ), 1,682 (4) (20 , 460), 1,660 (5) (40 , 71 , 550, 64 ), 1,522 (4) (442, 153, 13 ). Es bestehen enge strukturelle Beziehungen zwischen Johillerit und O'Danielit, Na(Zn, Mg)₃H₂(AsO₄)₃, sowie einigen synthetischen. Verbindungen.Johillerit ist violett durchscheinend. Die Spaltbarkeit nach {010} ist ausgezeichnet und nach {100} und {001} gut.H (Mohs)3.D=4,15 undD _X =4,21 g·cm^–3. Das Mineral ist optisch zweiachsig positiv, 2V80 (5)°. Die Werte der Lichtbrechung sindn =1,715 (4),n =1,743 (4) undn =1,783 (4). Die Auslöschung istn b und auf (010)n c16°. Johillerit ist stark pleochroitisch mit den AchsenfarbenX=violett-rot,Y = blauviolett undZ = grünblau. Das neue Mineral kommt in radialstrahligen Massen gemeinsam mit kupferhaltigem Adamin und Konichalcit in zersetzem Kupfererz von Tsumeb, Namibia, vor. Die Benennung erfolgte nach Prof. Dr.J.-E. Hiller (1911–1972).

---

Johillerite, Na(Mg, Zn) ₃ Cu(AsO ₄ ) ₃ , a new mineral from Tsumeb, Namibia

Summary Electron microprobe analysis of the new mineral johillerite gave Na₂O 5.4, MgO 18.3, ZnO 5.4, CuO 15.8, and As₂O₅ 55.8, total 100.7%. From this result, the ideal formula is given as Na(Mg, Zn)₃ Cu(AsO₄)₃. Johillerite crystallizes monoclinic,C2/c. The unit cell dimensions are:a=11.870(3),b=12.755 (3),c=6.770 (2) , =113.42 (2)°,Z=4. The strongest lines on the X-ray powder diffraction pattern are: 4,06 (5) (22 ), 3,50 (4) (310), 3,25 (8) (11 ), 2,75 (10) (330, 240), 2,64 (5) (311, 13 , 40 ), 1,952 (4) (13 , 35 ), 1,682 (4) (20 , 460), 1,660 (5) (40 , 71 , 550, 64 ), 1,522 (4) (442, 153, 13 ). There is a close relationship between johillerite, o'danielite, Na(Zn, Mg)₃H₂(AsO₄)₃, and some synthetic compounds. Johillerite is violet in colour, transparent. Cleavage is {010} perfect, {100} and {001} good.H (Mohs)3.D=4.15 andD _X =4.21 g·cm^–3. The mineral is optically biaxial positive, 2V80 (5)°. The refractive indices are:n =1.715 (4),n =1.743 (4),n =1.783 (4). The extinction isn b and on (010)n c16°. Strongly pleochroic with axial coloursX=violet-red,Y=bluish violet andZ=greenish blue. The new mineral was found in radiated masses together with cuprian adamite and conichalcite in an oxidized copper ore from Tsumeb, Namibia. It is named in honour of Prof. Dr.J.-E. Hiller (1911–1972).

---

---

Mit 1 Abbildung     

GEOSCIENCE 1989(VOL.3)CONTENTS

Sedimentary Suites(SDS)of Early St。la。P。nod in China………··、………M。ng Xiangkua。t al·(14).Meucd and ExamPles of Making maPs of World Reconstruu】onby a MlctocO*Puter·-·’··’··’·’…… ,……,……….、…………………………………………………··。,……··Li Xiang andZbang Lingkua(ZP)Geographic posit。on of the Qaidam Bio。k in L。ie Carboniferou。…·。…………·Li Yanpingetal.(32)Ontozenv of Homalophyllum Simpson,1900 and A SEM Study of itsMlcros发eletal 〕true…