GEO-ELECTRIC INVESTIGATION OF GROUNDWATER POTENTIAL IN LADERIN HOUSING ESTATE, ABEOKUTA, SOUTHWESTERN, NIGERIA

Vertical Electrical Sounding (VES) and 2D Electrical Resistivity Tomography (ERT), with Schlumberger and Wenner electrode array configurations respectively were employed to investigate the groundwater potential of Laderin Housing Estate located at Oke-mosan, Abeokuta, Ogun state, southwestern Nigeria. The area is underlain by the basement complex of the southwestern Nigeria. The research aimed at determining the aquifer/groundwater zone and characterizes the lithology of the study area. The geophysical survey involving nine VES and four profile of 2-D ERT lines with lengths varying from 100 m to 150 m were carried out. The field data from both the ERT and VES were processed and interpreted using RES2DINV and WINRESIST software respectively. Geometrical effects from the pseudo-section were removed and an image of true depth and true formation resistivity were produced. Three to four geo-electric layers were revealed in all, which are; topsoil, weathered layer, fractured and fresh basement rock. The result of 2 D inversion provide lithologic unit, weathering profile and geological structure favourable for groundwater potential. The results show that the basement rock was delineated with resistivity values that range between 701.3 Ωm and 9459.3 Ωm. The bedrock topography has a variable thickness of overburden between 3 m and above 16.4 m, which is fairly shallow. The geophysical survey show that VES 2, VES 3, VES 4, VES 5, and VES 6 are possible location for groundwater extraction. The difficult terrain, where thick overburden are located are also promising target for groundwater development.

Geochemistry and Mineralization of Some Selected Pegmatite Deposits in Panda North Central, Nigeria

Pegmatite constitutes an important lithologic unit in the Precambrian Basement Complex of Panda north central Nigeria. The primary aim of this study is to present a geochemical data of various rock types in the area especially pegmatite in order to determine their geochemical classification and mineralization potential of some selected pegmatite deposits in the area. Geochemical analysis reveals that the pegmatite samples have high SiO2 content; 73.8-94.8 wt%, low Na2O/K2O ratio suggesting they are strongly peralkaline and peraluminous, indicating that the pegmatite may have formed from mixed plutonic sources. The discrimination diagram of TiO2 versus SiO2 shows that the samples plotted on both igneous and sedimentary field, but majorly on the igneous field which is an implication that substantial material may have been generated from igneous sources. Also the plotting of the pegmatite samples in both the tholeiitic and calc-alkaline fields shows that the magma from which the rock was formed was not totally restricted in occurrence only to subduction related environment but also from the oceanic crust of calc-alkaline environments. This is further confirmed by discrimination diagrams plot of TiO2-K2O-P2O which indicates that substantial samples plotted fall within the continental crust. High potash content alkalies with relative Fe-enrichment and silica suggest the plutonic generation of magma and the development of the rocks in both the oceanic and continental crust. Major elements analysis of both the granitic rock aplite and biotite gneiss shows moderately high silica values. These values reflect the geochemical characteristic of crystalline rocks. The pegmatite of the study area exhibits low contents of Nb, Ta, Ga, Rb and Sn which are the major mineralization indices for pegmatite bodies. In classifying the pegmatites, rare metal indicative elements were used to discriminate the barren ones from the mineralized. A plot of Ta-Ga reveals that all the samples plotted are below the boundary of mineralization line, suggesting all the pegmatite samples in the study area to be barren in term of rare earth metals and can be compared to other pegmatite bodies in Nigeria and around the world.

Geochemical Characteristics of Amphibolites in Parts of Iseyin-Oyan Schist Belt, Southwestern Nigeria

Amphibolite is an important lithologic unit of the Nigerian basement complex that are commonly intercalated within metasedimentary sequences. Disseminated grains of sulphide minerals and base metal deposits are reported to occur in amphibolites and some other lithologies in other schist belts of Nigeria apart from the Iseyin-Oyan schist belt. Detailed geochemical study of amphibolitic rocks in this schist belt is scarce in literature, whereas none exist for the area under study, thus, this study is aimed at delineating the amphibolites within the Iseyin-Oyan schist belt around Itasa area with detail appraisal of their petrography and geochemical characteristics. A geologic field mapping was undertaken, and fresh representative amphibolite samples were obtained. Petrographic and geochemical studies of the samples were carried out with a view to understand their nature and petrogenetic characteristics. Geochemical data were elucidated using diverse geochemical discrimination diagrams. The amphibolites occur as lenses of small to large rocky boulders trending NNE-SSW and are essentially basal to quartz mica schist. Modal compositions revealed that they are dominantly composed of hornblende and plagioclase. XRD and mineral chemistry revealed that the plagioclase ranged from andesine to anorthite while hornblende is mainly magnesiohornblende. Geochemical data and discrimination diagrams revealed that the amphibolites are formed from basaltic to basaltic-andesite protolith that are of tholeiitic nature and had suffered crustal contamination. Tectonic discrimination diagrams indicated that the rocks were emplaced in the Mid Ocean Ridge but had been affected by collision due to Pan African Orogenic tectonic event.

Sequence stratigraphic framework of the mid-Cretaceous nonmarine Potomac Formation, New Jersey and Delaware

ABSTRACT We developed a sequence stratigraphic framework for the (Barremian to lower Cenomanian) fluvial–deltaic (primarily delta plain) Potomac Formation in the Medford, New Jersey, Fort Mott, New Jersey, and Summit Marina, Delaware coreholes. Previous studies have correlated distinctive lithologic units with attendant pollen zones and identified tentative sequence boundaries between lithologic units I (Barremian to lower Aptian, pollen Zone I), II (Aptian to lowermost Cenomanian, pollen Zone II), and III (lower Cenomanian, pollen Zone III) at all three sites. Here, we further subdivide these units into packages known as fluvial aggradation cycles (FACs). An analysis of FAC stacking patterns reveals potential sequence boundaries and systems tracts. FACs indicate that major lithologic unit boundaries are also sequence boundaries, indicate tentative higher-order sequence boundaries, and provide potential additional correlative surfaces among Potomac Formation sites. Our study demonstrates the applicability of the FAC method to identify stacking patterns and sequence stratigraphic surfaces in fluvial–deltaic deposits and demonstrates that FACs are excellent tools to decipher the difficult-to-correlate surfaces.

Seismic Mapping of Massive Dolomite Deposit Associated with Demise of MSC Salt Giant in Ionian Basin

<p>The origin of massive dolomite deposits has been an enduring and challenging problem for carbonate sedimentologists since the initial recognition of dolomite as a discrete carbonate mineral [CaMg(CO<sub>3</sub>)<sub>2</sub>]. The dolomite problem or enigma involves the fact that the mineral is very abundant in the geologic record, but it is rarely found forming in modern environments.  However, when modern dolomite is observed, it is generally, but not exclusively, found forming in hypersaline environments and in minor amounts.  Although the geologic record indicates that many ancient massive dolomite deposits formed in association with evaporites, modern examples of extensive amounts of dolomite being deposited under hypersaline conditions have not, or only rarely, been reported.   </p><p>One example of a massive hypersaline dolomite deposit of relatively recent origin may be the dolomite units associated with the end phase, at approximately 5.33 Ma, of the Messinian Salinity Crisis (MSC) in the Ionian Basin, Central Mediterranean (Hsü, Montadert, et al., 1978, Initial Reports of DSDP, Vol. 42, Part 1).  Drill core and interstitial waters obtained at DSDP Leg 42A, Site 374 in the Ionian abyssal plain revealed the presence of approximately 25 m of latest Miocene dolomitic mudstone (Lithologic Unit IIIa) capped by 8.5 m of earliest Pliocene dolomite (Lithologic Unit II).  Significantly, the pore-water geochemical data indicate that the dolomitization of the overlying earliest Pliocene nannofossil ooze may be an ongoing process.  Deeper drilling below the two dolomite units (Lithologic Unit II and IIIa) to the bottom of Site 374 recovered a further 29.5 m of gypsum/dolomitic mudstone cycles (Lithologic Unit IIIb) followed by 21 m of anhydrite and salts (Lithologic Unit IIIc).  Hence, the latest Miocene/earliest Pliocene dolomite sequence recovered at DSDP Site 374 is directly associated with the Messinian Salt Giant and potentially represents a massive dolomite deposit of an undetermined horizontal extent.</p><p>In order to measure the lateral dimensions of the combined dolomite/evaporite lithologic units in the central Ionian Sea, the University of Hamburg, using the facilities of the RV Meteor, conducted a multi-channel reflection seismic survey centered at DSDP Leg 42A, Site 374.  A powerful 6 kJoule sparker created the seismic signals, while a digital 144-channel streamer with an active length of 600 m recorded the data. The lowermost Pliocene reveals high lateral continuity and low reflection amplitudes, which is typical for the entire Pan-Mediterranean realm. The uppermost Messinian unit is characterized by a package of strong and positive reflection amplitudes (High Amplitude Reflection Package, HARP). The lateral continuity of the corresponding reflections is very low and the upper boundary is quite irregular. It is unlikely that the reflection configuration results from depositional processes, but it rather suggests diagenetic processes. We correlate the HARP with the dolomite- and gypsum-bearing sediments cored at DSDP Site 374 (Lithologic Unit IIIa, IIIb, IIIc), which is also consistent with the calculated depth. Based on preliminary estimates derived from the seismic survey, the areal extent of the dolomite deposit beneath the Ionian abyssal plain corresponds to a few 10’000 Km<sup>2</sup>, potentially representing a massive hypersaline dolomite deposit.</p>

Sedimentological Analysis of Core Samples to Decipher Depositional Environments: A Case Study of ‘Valz-01’ Well Niger-Delta Basin, Nigeria

Sedimentological studies of ninety-seven feet (97ft) of core, covering 1643 -1797.74 m from ‘Valz-01’ well Offshore Eastern Niger Delta was carried out using twenty-four (24) core slabbed samples with the aim of identifying the textural characterization of sediments from the various sectors of the lithologic unit and to determine the environment of deposition. Six lithofacies units were identified within the cored interval. They include: Muddy heterolith, laminated fine sandstone/siltstone, Fine sandstone/siltstone, Hummocky fine sandstone/siltstone, laminated shale sandy, and shale. Three depositional environments identified include marine environment, transitional and continental environment. The marine environment is characterized by the deposits of shale (1644.27 - 1709) m, while the continental environment is characterized by sandstone (1779 - 1781) m. The transitional environment is characterized by alternation of siltstone and shale (1643 – 1644.22 and 1781 – 1797.74) m. From the studies most of the analyzed samples are deposited in the delta influenced by fluvial and waves actions revealing beach sediments and turbidites.

Exceptional preservation of a Late Cretaceous dinosaur nesting site from Mongolia reveals colonial nesting behavior in a non-avian theropod

Colonial nesting behavior has been inferred in a variety of non-avian dinosaurs based on high concentrations of nests preserved in an area, but sedimentologic and taphonomic evidence demonstrating the contemporaneity of the nests is often lacking. A new nesting site discovered in the Upper Cretaceous Javkhlant Formation of the eastern Gobi Desert, Mongolia, preserves at least 15 egg clutches laid by a probable non-avian theropod, and provides strong evidence for colonial nesting in a non-avian dinosaur. The occurrence of the clutches at the top of a common paleosurface, the distribution of eggshell fragments within clutches, the presence of a consistent two-layer sediment infill within eggs, and a thin marker lithologic unit blanketing all the clutches indicate the clutches were laid and hatched in a single nesting season. Despite the absence of sedimentologic evidence indicative of nest structure, statistical analyses of egg characteristics and facies association reveal the clutches were likely incubated in covered or buried nests. Based on the number of hatched clutches, the hatching success rate of the colony was high (60%), similar to that of extant crocodylian populations and bird species that attend and/or protect their nests during the incubation period, which indicates nest attendance behavior in the Javkhlant theropods. Thus, colonial nesting with parental attendance, widespread in extant birds, likely evolved initially among non-brooding, non-avian dinosaurs to increase nesting success.

Inductive induced polarization effect in heliborne time-domain electromagnetic data for uranium exploration, northern part of Cuddapah Basin, India

The Peddagattu, Lambapur, Chitrial and Koppunuru uranium deposits along the northern margins of the Cuddapah Basin are confined to the middle Proterozoic unconformity interface between Archean basement granites and the overlying resistive quartzites. Negative transients observed in the coincident loop heliborne time-domain electromagnetic (HTEM) data over these deposits (occurring in outliers) are believed to be due to thick polarizable conductive zones occurring along the unconformity. Similar negative HTEM responses are recorded over the Gorukunta Tanda outlier. A ground spectral induced polarization (SIP) survey conducted over the outlier and ground geologic observations indicated an altered basement/regolith with thickness up to 5 m below 20–30 m thick quartzite. Interpretation of Cole-Cole parameters computed from the SIP data indicated a change in the dispersion. These Cole-Cole parameters were used in modeling negative HTEM data assuming a polarizable plate placed in a layered earth at a depth of approximately 50 m using the CSIRO LeroiAir program. A negative [Formula: see text] response in the late channels indicated that the negatives can be explained in terms of inductive induced polarization effects. Modeling of HTEM [Formula: see text] data for the profile through the Lambapur uranium deposit and the Gorukunta Tanda reveals the presence of a polarizable lithologic unit at a depth of approximately 40 m. This unit is interpreted as an argillic alteration of basement, with the presence of clay and/or disseminated sulfides as evidenced from the core extracted from the boreholes at depths below the highly resistive quartzite. Uranium mineralization is closely associated with altered basement and sulfides along the unconformity where the distinct negative electromagnetic (EM) signature is recorded. Furthermore, there exists a good correlation between the uranium mineralization grade and the thickness versus the averaged late-channel negative HTEM response over the known deposits. The negative EM response helped in locating the new target areas for uranium exploration.

GUNUNGAPI BAWAH LAUT KAWIO BARAT, PERAIRAN SANGIHE, SULAWESI UTARA: AKTIVITAS HIDROTERMAL DAN MINERALISASI

Ekspedisi INDEX-SATAL 2010 telah mengungkapkan fenomena aktivitas hidrotermal di bawah perairan barat Kepulauan Sangihe pada Gunungapi Bawah Laut Kawio Barat dengan puncaknya yang berada pada kedalaman laut sekitar 1860 m dan kakinya pada kedalaman sekitar 5400 m. Penyelaman ROV (Remotely Operated Vehicle) Little Hercules di Gunungapi Kawio Barat yang dipusatkan di sisi baratlaut dari puncak gunung menyapu mulai kedalaman 3000 m hingga menuju ke arah puncak pada kedalaman 1860 m. Kelompok batuan dicirikan oleh bongkahan lava yang sudah pecah ditutupi sedimen halus berwarna abu-abu cerah; sedangkan pada sisi tenggara umumnya ditempati aliran lava bantal. Pada sisi baratdaya, tempat lembah dalam menoreh Gunungapi Kawio Barat dijumpai kepulan asap dari lereng bagian bawah yang akhirnya pada kedalaman sekitar 1890 m dijumpai aktivitas hidrotermal bawah laut yang merupakan suatu fenomena yang pertama kali direkam langsung dari bawahlaut perairan Indonesia. Fenomena yang terekam berupa pemunculan asap (smokers) di sepanjang rekahan (fissures), dicirikan oleh warna asap yang bervariasi dari putih, kuning atau abu-abu cerah yang kemungkinan menunjukkan indikasi perbedaan komposisi kimiawi dari fluida hidrotermal. Selain asap, teramati juga adanya gelembung cairan (panas) atau bubbles dari rekahan. Penemuan baru lainnya adalah adanya fluida hidrotermal muncul ke permukaan dan membentuk suatu cerobong hidrotermal atau chimney di daerah yang secara tektonik dikontrol oleh konvergensi lempeng. Batuan-batuan di sekitar rekahan hidrotermal (hydrothermal vent) umumnya telah terubah dengan dominasi warna putih hingga kelabu. Di sekitar rekahan hidrotermal diendapkan belerang berwarna kuning kehitaman. Mineralisasi kemungkinan terjadi di sekitar cerobong hidrotermal, terakumulasi membentuk endapan mineral yang ditunjukkan oleh warna coklat, abu-abu, dan kemerahan. Hal ini terutama teramati di sekitar cerobong yang sudah tidak mengeluarkan gelembung atau asap, serta dijumpai kehadiran endapan serakan butiran batuan atau mineral berwarna coklat atau hitam. Kata kunci: INDEX-SATAL 2010, aktivitas hidrotermal, ROV, asap hidrotermal, gelembung cairan, cerobong hidrotermal, konvergensi lempeng, mineralisasi INDEX-SATAL Expedition 2010 has revealed the phenomenon of hydrothermal activity in the western part of the Sangihe Waters in Kawio Barat Submarine Volcano with the peak which is located at 1860 m depths and the bottom at about 5400 m depths. A ROV (Remotely Operated Vehicle) "Little Hercules" dive in Kawio Barat was centered on the northwest side of the mountain began to sweep from the depths of 3000 m toward the top of 1860 m depths. The lithologic unit is characterized by the present of broken lavas covered with fine grey colored sediment whilist in the southeast side is composed of pillows lavas. In the southwest side, in which the deep valleys incise Kawio Barat, a clouds of smoke from the lower slopes are observed; finally at 1890 m depths a submarine hydrothermal activity is noted. This phenomenon represents the first submarine direct record made from the bottom of the Indonesian Waters. Those smokers phenomena are recorded along fissures, characterized by various colors of white, yellow to grey due to different chemical composition of hydrothermal fluids. Besides, the hot bubbles are also arised from the fissures. The other new discovery is the presence of hydrothermal chimney in the area of tectonically controlled by convergence plates. Rocks surrounding the hydrothermal vents are generally altered giving grey to white colors and the presence of dark yellow sulfur deposits. Mineralization may occur and accumulated in hydrothermal chimney and its surrounding to form brown-, grey-, and reddish- color deposits The latter are commonly found in inactive chimneys, indicated by the presence of dispersed brown and black color grains/chips of both sedimentary rocks or minerals as well. Keywords: INDEX-SATAL 2010, hydrothermal activity, ROV, hydrothermal smokers, bubbles, hydrothermal chimney, plate convergence, mineralization